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• 3181. [Image] Water quality conditions in Upper Klamath and Agency Lakes, Oregon, 2005

  	Agency Lakes. Oregon. 2005 M.Wood By Gene R. Hoilman, Mary K. Lindenberg, and Tamara Abstract During June-October 2005, water quality data were collected from Upper Klamath and Agency Lakes In Oregon, ...
  	Citation × Citation Citation Abstract Copy Title: Water quality conditions in Upper Klamath and Agency Lakes, Oregon, 2005 Author: Hoilman, Gene R Year: 2008 Agency Lakes. Oregon. 2005 M.Wood By Gene R. Hoilman, Mary K. Lindenberg, and Tamara Abstract During June-October 2005, water quality data were collected from Upper Klamath and Agency Lakes In Oregon, and meteorological data were collected around and within Upper Klamath Lake. Data recorded at two continuous water quality monitors In Agency Lake showed similar temperature patterns throughout the field season, but data recorded at the northern site showed more day-to-day variability for dissolved oxygen concentration and saturation after late June and more day-to-day variability for pH and specific conductance values after mid-July. Data recorded from the northern and southern parts of Agency Lake showed more comparable day-to-day variability in dissolved oxygen concentrations and pH from September through the end of the monitoring period. For Upper Klamath Lake, seasonal (late July through early August) lows of dissolved oxygen concentrations and saturation were coincident with a seasonal low of pH values and seasonal highs of ammonia and orthophosphate concentrations, specific conductance values, and water temperatures. Patterns in these parameters, excluding water temperature, were associated with bloom dynamics of the cyanobacterium (blue-green alga) Aphanizomenonflos-aquae in Upper Klamath Lake. In Upper Klamath Lake, water temperature in excess of 28 degrees Celsius (a high stress threshold for Upper Klamath Lake suckers) was recorded only once at one site during the field season. Large areas of Upper Klamath Lake had periods of dissolved oxygen concentration of less than 4 milligrams per liter and pH value greater than 9.7, but these conditions were not persistent throughout days at most sites. Dissolved oxygen concentrations in Upper Klamath Lake on time scales of days and months appeared to be influenced, in part, by bathymetry and prevailing current flow patterns. Diel patterns of water column stratification were evident, even at the deepest sites. This diel pattern of stratification was attributable to diel wind speed patterns and the shallow nature of most of Upper Klamath Lake. Timing of the daily extreme values of dissolved oxygen concentration, pH, and water temperature was less distinct with increased water column depth. Chlorophyll a concentrations varied spatially and temporally throughout Upper Klamath Lake. Location greatly affected algal concentrations, in turn affecting nutrient and dissolved oxygen concentrations—some of the highest chlorophyll a concentrations were associated with the lowest dissolved oxygen concentrations and the highest un-ionized ammonia concentrations. The occurrence of the low dissolved oxygen and high un-ionized ammonia concentrations coincided with a decline in algae resulting from cell death, as rn.easu.red by concentrations of chlorophyll a. Dissolved oxygen production, rates in. experim.en.ts were as high as 1.47 milligrams of oxygen per liter per hour, and consumption rates were as much as -0.73 milligrams of oxygen per liter per hour. Dissolved oxygen, consumption rates measured in. this study were comparable to those measured in a 2002 Upper Klamath Lake study, and a higher rate of dissolved oxygen consumption was recorded in. dark bottles positioned higher in the water column. Data, though, inconclusive, indicated that a decreasing trend of dissolved oxygen productivity through July could have contributed to the decreasing dissolved oxygen concentrations and percent saturation recorded in Upper Klamath Lake during this time. Phytoplankton self-shading was evident from, a general inverse relation between depth of photic zone and chlorophyll a concentrations. This shading caused net dissolved oxygen consumption during daylight hours in lower parts of the water column that would otherwise have been in the photic zone. Meteorological data collected in and around Upper Klamath Lake showed that winds were likely to come from a broad range of westerly directions in the northern one-third of the lake, but tended to come from a narrow range of northwesterly directions over the main body of the lake farther south. Title: Water quality conditions in Upper Klamath and Agency Lakes, Oregon, 2005 Author: Hoilman, Gene R Year: 2008 Agency Lakes. Oregon. 2005 M.Wood By Gene R. Hoilman, Mary K. Lindenberg, and Tamara Abstract During June-October 2005, water quality data were collected from Upper Klamath and Agency Lakes In Oregon, and meteorological data were collected around and within Upper Klamath Lake. Data recorded at two continuous water quality monitors In Agency Lake showed similar temperature patterns throughout the field season, but data recorded at the northern site showed more day-to-day variability for dissolved oxygen concentration and saturation after late June and more day-to-day variability for pH and specific conductance values after mid-July. Data recorded from the northern and southern parts of Agency Lake showed more comparable day-to-day variability in dissolved oxygen concentrations and pH from September through the end of the monitoring period. For Upper Klamath Lake, seasonal (late July through early August) lows of dissolved oxygen concentrations and saturation were coincident with a seasonal low of pH values and seasonal highs of ammonia and orthophosphate concentrations, specific conductance values, and water temperatures. Patterns in these parameters, excluding water temperature, were associated with bloom dynamics of the cyanobacterium (blue-green alga) Aphanizomenonflos-aquae in Upper Klamath Lake. In Upper Klamath Lake, water temperature in excess of 28 degrees Celsius (a high stress threshold for Upper Klamath Lake suckers) was recorded only once at one site during the field season. Large areas of Upper Klamath Lake had periods of dissolved oxygen concentration of less than 4 milligrams per liter and pH value greater than 9.7, but these conditions were not persistent throughout days at most sites. Dissolved oxygen concentrations in Upper Klamath Lake on time scales of days and months appeared to be influenced, in part, by bathymetry and prevailing current flow patterns. Diel patterns of water column stratification were evident, even at the deepest sites. This diel pattern of stratification was attributable to diel wind speed patterns and the shallow nature of most of Upper Klamath Lake. Timing of the daily extreme values of dissolved oxygen concentration, pH, and water temperature was less distinct with increased water column depth. Chlorophyll a concentrations varied spatially and temporally throughout Upper Klamath Lake. Location greatly affected algal concentrations, in turn affecting nutrient and dissolved oxygen concentrations—some of the highest chlorophyll a concentrations were associated with the lowest dissolved oxygen concentrations and the highest un-ionized ammonia concentrations. The occurrence of the low dissolved oxygen and high un-ionized ammonia concentrations coincided with a decline in algae resulting from cell death, as rn.easu.red by concentrations of chlorophyll a. Dissolved oxygen production, rates in. experim.en.ts were as high as 1.47 milligrams of oxygen per liter per hour, and consumption rates were as much as -0.73 milligrams of oxygen per liter per hour. Dissolved oxygen, consumption rates measured in. this study were comparable to those measured in a 2002 Upper Klamath Lake study, and a higher rate of dissolved oxygen consumption was recorded in. dark bottles positioned higher in the water column. Data, though, inconclusive, indicated that a decreasing trend of dissolved oxygen productivity through July could have contributed to the decreasing dissolved oxygen concentrations and percent saturation recorded in Upper Klamath Lake during this time. Phytoplankton self-shading was evident from, a general inverse relation between depth of photic zone and chlorophyll a concentrations. This shading caused net dissolved oxygen consumption during daylight hours in lower parts of the water column that would otherwise have been in the photic zone. Meteorological data collected in and around Upper Klamath Lake showed that winds were likely to come from a broad range of westerly directions in the northern one-third of the lake, but tended to come from a narrow range of northwesterly directions over the main body of the lake farther south. Close

• 3182. [Image] Macroecology, paleoecology, and ecological integrity of terrestrial species and communities of the interior Columbia River basin and northern portions of the Klamath and Great Basins

  	This report presents information on biogeography and broad-scale ecology (macroecology) of selected fungi, lichens, bryophytes, vascular plants, invertebrates, and vertebrates of the interior Columbia ...
  	Citation × Citation Citation Abstract Copy Title: Macroecology, paleoecology, and ecological integrity of terrestrial species and communities of the interior Columbia River basin and northern portions of the Klamath and Great Basins Author: U.S. Department of Agriculture. Forest Service. Pacific Northwest Research Station; U.S.Department of the Interior. Bureau of Land Management. Year: 1998, 2006, 2005 This report presents information on biogeography and broad-scale ecology (macroecology) of selected fungi, lichens, bryophytes, vascular plants, invertebrates, and vertebrates of the interior Columbia River basin and adjacent areas. Rare plants include many endemics associated with local conditions. Potential plant and invertebrate bioindicators are identified. Species ecological functions differ among communities and variously affect ecosystem diversity and productivity. Species of alpine and subalpine communities are identified that may be at risk from climate change. Maps of terrestrial ecological integrity are presented. Keywords: Macroecology, paleoecology, ecological integrity, terrestrial communities, ecosystems, wildlife, fungi, lichens, bryophytes, vascular plants, invertebrates, arthropods, mollusks, amphibians, reptiles, birds, mammals, endemism, interior Columbia River basin, Klamath Basin, Great Basin. Title: Macroecology, paleoecology, and ecological integrity of terrestrial species and communities of the interior Columbia River basin and northern portions of the Klamath and Great Basins Author: U.S. Department of Agriculture. Forest Service. Pacific Northwest Research Station; U.S.Department of the Interior. Bureau of Land Management. Year: 1998, 2006, 2005 This report presents information on biogeography and broad-scale ecology (macroecology) of selected fungi, lichens, bryophytes, vascular plants, invertebrates, and vertebrates of the interior Columbia River basin and adjacent areas. Rare plants include many endemics associated with local conditions. Potential plant and invertebrate bioindicators are identified. Species ecological functions differ among communities and variously affect ecosystem diversity and productivity. Species of alpine and subalpine communities are identified that may be at risk from climate change. Maps of terrestrial ecological integrity are presented. Keywords: Macroecology, paleoecology, ecological integrity, terrestrial communities, ecosystems, wildlife, fungi, lichens, bryophytes, vascular plants, invertebrates, arthropods, mollusks, amphibians, reptiles, birds, mammals, endemism, interior Columbia River basin, Klamath Basin, Great Basin. Close

• 3183. [Image] Biological assessment of Klamath Project's continuing operations on the endangered Lost River sucker and shortnose sucker

  	BIOLOGICAL ASSESSMENT OF KLAMATH PROJECT'S CONTINUING OPERATIONS ON THE ENDANGERED LOST RIVER SUCKER AND SHORTNOSE SUCKER U.S. Bureau of Reclamation Mid-Pacific Region Klamath Basin Area Office Klamath ...
  	Citation × Citation Citation Abstract Copy Title: Biological assessment of Klamath Project's continuing operations on the endangered Lost River sucker and shortnose sucker Author: United States. Bureau of Reclamation Year: 2001, 2005 BIOLOGICAL ASSESSMENT OF KLAMATH PROJECT'S CONTINUING OPERATIONS ON THE ENDANGERED LOST RIVER SUCKER AND SHORTNOSE SUCKER U.S. Bureau of Reclamation Mid-Pacific Region Klamath Basin Area Office Klamath Falls, Oregon February 13,2001 TABLE OF CONTENTS 1.0 INTRODUCTION 2 2.0 DESCRIPTION OF THE ACTION 3 3.0 DESCRIPTION OF HISTORIC OPERATIONS 6 4.0 ENDANGERED SPECIES POTENTIALLY AFFECTED BY THE KLAMATH PROJECT 16 5.0 ENVIRONMENTAL BASELINE 60 6.0 EFFECTS OF KLAMATH PROJECT ON BALD EAGLES 60 7.0 EFFECTS OF KLAMATH PROJECT ENDANGERED SUCKERS 63 8.0 PROPOSED CRITICAL HABITAT FOR ENDANGERED SUCKERS 82 9.0 CUMULATIVE EFFECTS 84 10.0 DETERMINATION OF EFFECTS 89 11.0 LITERATURE CITED 90 12.0 PERSONAL COMMUNICATIONS 100 13.0 APPENDIX 1 - ESA CONSULTATION REVIEW 101 Title: Biological assessment of Klamath Project's continuing operations on the endangered Lost River sucker and shortnose sucker Author: United States. Bureau of Reclamation Year: 2001, 2005 BIOLOGICAL ASSESSMENT OF KLAMATH PROJECT'S CONTINUING OPERATIONS ON THE ENDANGERED LOST RIVER SUCKER AND SHORTNOSE SUCKER U.S. Bureau of Reclamation Mid-Pacific Region Klamath Basin Area Office Klamath Falls, Oregon February 13,2001 TABLE OF CONTENTS 1.0 INTRODUCTION 2 2.0 DESCRIPTION OF THE ACTION 3 3.0 DESCRIPTION OF HISTORIC OPERATIONS 6 4.0 ENDANGERED SPECIES POTENTIALLY AFFECTED BY THE KLAMATH PROJECT 16 5.0 ENVIRONMENTAL BASELINE 60 6.0 EFFECTS OF KLAMATH PROJECT ON BALD EAGLES 60 7.0 EFFECTS OF KLAMATH PROJECT ENDANGERED SUCKERS 63 8.0 PROPOSED CRITICAL HABITAT FOR ENDANGERED SUCKERS 82 9.0 CUMULATIVE EFFECTS 84 10.0 DETERMINATION OF EFFECTS 89 11.0 LITERATURE CITED 90 12.0 PERSONAL COMMUNICATIONS 100 13.0 APPENDIX 1 - ESA CONSULTATION REVIEW 101 Close

• 3184. [Image] The Chemical and biological impact of Klamath Marsh on the Williamson River, Oregon

  	A comparative study of the Williamson River (before and after passage through Klamath Marsh) and the Sprague River (which is a major tributary of the Williamson River) in South Central Oregon has provided ...
  	Citation × Citation Citation Abstract Copy Title: The Chemical and biological impact of Klamath Marsh on the Williamson River, Oregon Author: Perdue, Edward M. Year: 1981, 2005 A comparative study of the Williamson River (before and after passage through Klamath Marsh) and the Sprague River (which is a major tributary of the Williamson River) in South Central Oregon has provided substantial insight into the effects of a marsh environment on the transport of iron and aquatic humus in river water. In the Sprague River and in the pre-marsh Williamson River, iron is transported primarily as 0.80 ym suspended particulate material. In Klamath Marsh, this coarse particulate material is "weathered11, yielding iron-aquatic humus "complexes'1. Thus, most iron and aquatic humus in the post-marsh Williamson River are in the 0.025 ?m size fraction. Presumably, other trace metals would be similarly affected. Klamath Marsh serves as an important source of biologically derived solutes such as amino acids and sugars. Fractionation studies have shown that amino acids are almost exclusively humic-bound in the Will-iamson River system, while sugars may be present as either polysacchar-ides (PS) or humic-bound saccharides (HS). The PS/HS ratio may reflect the relative importance of autochthonous and allochthonous sources of sugars. Major solute composition strongly indicates that ground waters flowing into the pre-marsh Williamson River and the Sprague River are derived from a different source than are ground waters which enter the post-marsh Williamson River from Big Springs, Spring Creek, and from unidentified springs below Klamath Marsh. Nutrient concentrations (H4SiO4, NO3, PO43) are significantly higher in spring waters than elsewhere in the system. While nitrate levels (3-11 ?m) were somewhat low, phosphate levels (1-3 ?m) were quite high throughout the Williamson River system. There was some evidence for nitrogen limitation of algal growth in the pre-marsh Williamson River. While Fragilaria construens was dominant throughout the Williamson River system, several Navicula spp. were restricted to the pre-marsh Williamson River and several Fragilaria spp. and Nitzschia, spp. were found only in the post-marsh Williamson River. In Upper Klamath Lake, Stephanodiscus astrea minuta, Fragilaria construens, and Aphanizomenon flos-aquae appeared in succession, with nuisance blooms of the latter organism occurring July-November. The cessation of flow of humic-rich water from Klamath Marsh during the summer months drastically decreased the flux of aquatic humus, iron, amino acids, and other marsh-derived solutes in the post-marsh Williamson River. At the time of cessation of flow from Klamath Marsh, nuisance blooms of Aphanizomenon flos-aquae appeared in Upper Klamath Lake. Furthermore, when flow from the marsh was re-established with the first major winter rains in November or December, Aphanizomenon flos-aquae abruptly ceased to grow in Upper Klamath Lake. Further studies are planned to determine whether this correlation is causal or coincidental. Title: The Chemical and biological impact of Klamath Marsh on the Williamson River, Oregon Author: Perdue, Edward M. Year: 1981, 2005 A comparative study of the Williamson River (before and after passage through Klamath Marsh) and the Sprague River (which is a major tributary of the Williamson River) in South Central Oregon has provided substantial insight into the effects of a marsh environment on the transport of iron and aquatic humus in river water. In the Sprague River and in the pre-marsh Williamson River, iron is transported primarily as 0.80 ym suspended particulate material. In Klamath Marsh, this coarse particulate material is "weathered11, yielding iron-aquatic humus "complexes'1. Thus, most iron and aquatic humus in the post-marsh Williamson River are in the 0.025 ?m size fraction. Presumably, other trace metals would be similarly affected. Klamath Marsh serves as an important source of biologically derived solutes such as amino acids and sugars. Fractionation studies have shown that amino acids are almost exclusively humic-bound in the Will-iamson River system, while sugars may be present as either polysacchar-ides (PS) or humic-bound saccharides (HS). The PS/HS ratio may reflect the relative importance of autochthonous and allochthonous sources of sugars. Major solute composition strongly indicates that ground waters flowing into the pre-marsh Williamson River and the Sprague River are derived from a different source than are ground waters which enter the post-marsh Williamson River from Big Springs, Spring Creek, and from unidentified springs below Klamath Marsh. Nutrient concentrations (H4SiO4, NO3, PO43) are significantly higher in spring waters than elsewhere in the system. While nitrate levels (3-11 ?m) were somewhat low, phosphate levels (1-3 ?m) were quite high throughout the Williamson River system. There was some evidence for nitrogen limitation of algal growth in the pre-marsh Williamson River. While Fragilaria construens was dominant throughout the Williamson River system, several Navicula spp. were restricted to the pre-marsh Williamson River and several Fragilaria spp. and Nitzschia, spp. were found only in the post-marsh Williamson River. In Upper Klamath Lake, Stephanodiscus astrea minuta, Fragilaria construens, and Aphanizomenon flos-aquae appeared in succession, with nuisance blooms of the latter organism occurring July-November. The cessation of flow of humic-rich water from Klamath Marsh during the summer months drastically decreased the flux of aquatic humus, iron, amino acids, and other marsh-derived solutes in the post-marsh Williamson River. At the time of cessation of flow from Klamath Marsh, nuisance blooms of Aphanizomenon flos-aquae appeared in Upper Klamath Lake. Furthermore, when flow from the marsh was re-established with the first major winter rains in November or December, Aphanizomenon flos-aquae abruptly ceased to grow in Upper Klamath Lake. Further studies are planned to determine whether this correlation is causal or coincidental. Close

• 3185. [Image] Histopathological changes in gills of Lost River suckers (Deltistes luxatus) exposed to elevated ammonia and elevated pH

  	Lease, Hilary M., Histopathological Changes in Gills of Lost River Suckers (Deltistes luxatus) Exposed to Elevated Ammonia and Elevated pH, M.S., Department of Zoology and Physiology, December, 2000. ...
  	Citation × Citation Citation Abstract Copy Title: Histopathological changes in gills of Lost River suckers (Deltistes luxatus) exposed to elevated ammonia and elevated pH Author: Lease, Hilary Marian Year: 2000, 2008, 2005 Lease, Hilary M., Histopathological Changes in Gills of Lost River Suckers (Deltistes luxatus) Exposed to Elevated Ammonia and Elevated pH, M.S., Department of Zoology and Physiology, December, 2000. The Lost River sucker {Deltistes luxatus) is a federally listed, endangered fish species endemic to Upper Klamath Lake?a large, shallow hypereutrophic lake in southern Oregon. Sucker population declines in the lake over the past few decades are thought to be partly attributable to extreme water quality conditions, including elevated ammonia concentrations and elevated pH, that occur during summer cyanobacterial blooms. I analyzed structural changes in gills of larval Lost River suckers after they were exposed to elevated pH and elevated ammonia concentrations in chronic toxicity tests conducted in the laboratory. Histopathological changes in sucker lamellae were observed at ammonia concentrations that did not significantly decrease survival, growth, whole-body ion content, or swimming performance. Structural changes that I evaluated included O2 diffusion distance, lamellar thickness, hyperplasic and hypertrophic mucous cells, and infiltration of white blood cells into the lymphatic space. The increases in diffusion distance and lamellar thickness were statistically significant (P < 0.05). These gill changes are indicative of potentially compromised respiratory and ionoregulatory capacity. Because in this species gill structural changes appear to be a more sensitive indicator of stress in eutrophic water quality conditions than are the more traditional sublethal indices, gill histopathology might be useful for monitoring the health of Lost River suckers in Upper Klamath Lake. Title: Histopathological changes in gills of Lost River suckers (Deltistes luxatus) exposed to elevated ammonia and elevated pH Author: Lease, Hilary Marian Year: 2000, 2008, 2005 Lease, Hilary M., Histopathological Changes in Gills of Lost River Suckers (Deltistes luxatus) Exposed to Elevated Ammonia and Elevated pH, M.S., Department of Zoology and Physiology, December, 2000. The Lost River sucker {Deltistes luxatus) is a federally listed, endangered fish species endemic to Upper Klamath Lake?a large, shallow hypereutrophic lake in southern Oregon. Sucker population declines in the lake over the past few decades are thought to be partly attributable to extreme water quality conditions, including elevated ammonia concentrations and elevated pH, that occur during summer cyanobacterial blooms. I analyzed structural changes in gills of larval Lost River suckers after they were exposed to elevated pH and elevated ammonia concentrations in chronic toxicity tests conducted in the laboratory. Histopathological changes in sucker lamellae were observed at ammonia concentrations that did not significantly decrease survival, growth, whole-body ion content, or swimming performance. Structural changes that I evaluated included O2 diffusion distance, lamellar thickness, hyperplasic and hypertrophic mucous cells, and infiltration of white blood cells into the lymphatic space. The increases in diffusion distance and lamellar thickness were statistically significant (P < 0.05). These gill changes are indicative of potentially compromised respiratory and ionoregulatory capacity. Because in this species gill structural changes appear to be a more sensitive indicator of stress in eutrophic water quality conditions than are the more traditional sublethal indices, gill histopathology might be useful for monitoring the health of Lost River suckers in Upper Klamath Lake. Close

• 3186. [Image] Annual program summary 2004

  	Annual Program Summary and Monitoring Report - FY2004 Table of Contents ANNUAL PROGRAM SUMMARY 1.0 Introduction 3 2.0 Summary of Accomplishments 3 3.0 Budget and Employment 6 4.0 Land ...
  	Citation × Citation Citation Abstract Copy Title: Annual program summary 2004 Author: United States. Bureau of Land Management. Klamath Falls Resource Area Office District Year: 2005 Annual Program Summary and Monitoring Report - FY2004 Table of Contents ANNUAL PROGRAM SUMMARY 1.0 Introduction 3 2.0 Summary of Accomplishments 3 3.0 Budget and Employment 6 4.0 Land Use Allocations within the Klamath Falls Resource Area 6 Late-Successional Reserves and Assessments 8 Matrix 8 5.0 Aquatic Conservation Strategy 9 Riparian Reserves 9 Watershed Analysis and Key Watersheds 9 Watershed Restoration 10 Roads 10 Riparian Habitat Enhancement 10 Stream Restoration 11 6.0 Air Quality 11 7.0 Water and Soils 11 Water - Project Implementation 11 Soils - Project Implementation 12 Water - Inventory and Monitoring 12 Soils -Inventory and Monitoring 13 State-listed Clean Water Act 303d Streams 13 RMP Best Management Practices 13 8.0 Terrestrial Species and Habitat Management 14 Survey and Manage Species 14 Threatened/Endangered Species 14 Northern Spotted Owl 14 Bald Eagle 14 Special Status Species-Animals 15 Peregrine Falcon 15 Yellow Rails 15 Bats 15 Northern Goshawk 15 Oregon Spotted Frog 15 Sage Grouse 16 vii Klamath Falls Resource Area Mollusks 16 Great Gray Owl 16 Special Status Species - Plants 16 Other Species of Concern 17 Neotropical Migratory Landbirds 17 Terrestrial Habitat Management 17 Nest Sites, Activity Centers, and Rookeries 17 Big Game Habitat 19 9.0 Aquatic Species and Habitat Management 19 Threatened/Endangered Species 19 Lost River and Shortnose Suckers 19 Bull Trout 20 Endangered Species Act Consultation 20 Aquatic Habitat Restoration 20 Klamath River Hydroelectric Facility Relicensing 21 10.0 Pathogen, Disease, and Pest Management 21 11.0 Weed Management 22 Inventories 22 Control 22 12.0 Special Areas/Management 23 Wild and Scenic Rivers 23 Wilderness 23 Areas of Critical Environmental Concern 23 Tunnel Creek Special Botanical Area 24 Klamath Canyon ACEC 24 Old Baldy Research Natural Area 24 Wood River Wetland ACEC 24 Environmental Education Areas 25 13.0 Cultural Resources 26 14.0 Visual Resources 26 15.0 Rural Interface Areas 26 16.0 Socioeconomic Conditions 27 Jobs-in-the-Woods 28 17.0 Environmental Justice 30 18.0 Recreation 30 Recreation Pipeline Restoration Funds 30 Recreation Projects 31 viii Annual Program Summary and Monitoring Report - FY2004 Recreation Fee Demonstration Project 31 Status of Recreation Plans 32 Volunteer Activities 32 Tourism 33 19.0 Forest Management and Timber Resources 33 Silvicultural Prescriptions 33 Timber Sale Planning 34 FY 2004 Timber Sale Accomplishments 34 Status of Sold & Awarded Klamath Falls RMP Timber Sales 35 Forest Development Activities 39 Stewardship Contracting 42 20.0 Special Forest Products 42 21.0 Energy and Minerals 43 22.0 Land Tenure Adjustments 44 23.0 Access and Rights-of-Way 45 24.0 Transportation and Roads 45 25.0 Hazardous Materials 46 26.0 Wildfire/Fuels Management 46 27.0 Law Enforcement 47 28.0 Rangeland Resources / Grazing Management 48 Fiscal Year 2004 Summary 49 Fiscal Years 1996-2004 Summary 50 Wild Horse Management 51 29.0 Cadastral Survey 52 30.0 Education and Outreach 52 31.0 Research 56 32.0 Coordination and Consultation 58 Federal Agencies 58 State of Oregon 58 Counties 59 Cities 59 Tribes 59 IX Klamath Falls Resource Area Watershed Councils 59 Chartered Advisory Groups 60 Other Local Coordination and Cooperation 61 33.0 National Environmental Policy Act Analysis and Documentation 63 NEPA documentation 63 Klamath Falls Resource Area Environmental Documentation 63 Protests and Appeals 63 34.0 Plan Evaluations 64 Third Year Evaluation 64 Eighth Year Evaluation 64 35.0 Plan Maintenance 65 36.0 Plan Amendments 72 Plan Revision 76 MONITORING REPORT Introduction 79 All Land Use Allocations 83 Late-Successional Reserves 86 Matrix 88 Riparian Reserves 92 Air Quality 95 Water and Soils 96 Terrestrial Species Habitat 101 Special Status and SEIS Special Attention Species Habitat 106 Aquatic Species Habitat 110 Noxious Weeds 112 Special Areas 113 Wild and Scenic Rivers 115 Cultural Resources Including American Indian Values 116 Visual Resources 118 Rural Interface Areas 119 Socioeconomic Conditions 120 Recreation 121 Forest Management and Timber Resources 121 Special Forest/Natural Products 122 Wildfire / Fuels Management 124 Rangeland Resources / Grazing Management 124 GLOSSARY/ACRONYMS 129 Annual Program Summary and Monitoring Report - FY2004 List of Tables Table 2.1 - Summary of Resource Management Actions, Directions, and Accomplishments 4 Table 2.1 - Summary of Resource Management Actions, Directions, and Accomplishments (Cont.).5 Table 3.1 - Resource Area Budget Fiscal Year 2004 6 Table 4.1 - Land Use Allocation 8 Table 5.1 - Watershed Analysis Schedule 10 Table 5.2-Watershed Analysis Status Fiscal Year 2004 10 Table 6.1 -Air Quality Management Fiscal Year 2004 11 Table 7.1 - Watershed Activity Fiscal Year 2004 12 Table 7.2 - KFRA Clean Water Act 303(d) Water Bodies 13 Table 8.1a - BLM /KFRA Special Status Species Designations Summary -Animals 18 Table 8.1b - BLM (KFRA) Special Status Species Designations Summary - Plants 18 Table 8.2 - Terrestrial Habitat Monitoring Fiscal Year 2004 18 Table 8.3 - Monitoring for Nest Sites, Activity Centers, Rookeries, Special Habitats 18 Table 9.1 -Aquatic Habitat/ Fish Passage Management Fiscal Year 2004 19 Table 11.1 - Managed Weed Species 20 Table 12.1 - Special Management Areas 25 Table 13.1 - Cultural Resources Management Fiscal Year 2004 26 Table 16.1 - Total Payments in Lieu of Taxes and Acres by County for FY 2004 28 Table 16.2 - O&C Payments To Counties FY 2004 29 Table 16.3 - Jobs in the Woods Program Fiscal Year 2004 29 Table 18.1 - Recreation Statistics Fiscal Year 2004 30 Table 18.2 - Recreation Fee Demonstration Project Fiscal Year 2004 32 Table 19.1 - Klamath Falls Timber Sale Volume (MBF) and Acres FY 2004 35 Table 19.2-Timber Volume Sold in FY 2004 36 Table 19.3 - Harvest Activity for FY 2004 36 Table 19.4 - Planned Timber Sales (FY 2005 & 2006) 36 Table 19.5 - Status of Sold and Awarded Timber Sales 37 Table 19.6 - Summary of Volume Sold 38 Table 19.7 -Volume and Acres Sold by Allocations 38 Table 19.8 - Timber Sales Sold by Harvest Types 38 Table 19.9 - Timber Sale Acres Sold by Age Class 39 Table 19.10 - Forest Development Activities 41 Table 20.1 - Special Forest Products Fiscal Year 2004 43 Table 21.1 - Energy and Minerals Management Fiscal Year 2004 44 Table 22.1 - Land Use Tenure Adjustments Fiscal Year 2004 45 Table 24.1 - Roads and Transportation Management Fiscal Year 2004 45 Table 25.1 - Hazardous Materials Management Fiscal Year 2004 46 Table 26.1 - Fire and Fuels Management Fiscal Year 2004 46 Table 27.1 - Law Enforcement Fiscal Year 2004 47 Table 28.1 - Range Resources Management Fiscal Year 2004 48 Table 29.1 -Cadastral Survey Summary Fiscal Year 2004 52 Table 30.1 - Environmental Education/Outreach Program Summary FY2004 54 Table 30.2 - Environmental Education/Outreach Special Events FY2004 55 Table 30.3 - Environmental Education/Outreach Programs & Tours FY 2004 56 Table 32.1 - Challenge Cost Share Fiscal Year 2004 62 XI Klamath Falls Resource Area Table 33.1 - NEPA Analyses and Documentation Fiscal Year 2004 64 Table 36.1 - Redefined Survey and Manage Categories 74 Table M.I - Projects Monitored FY 2004 80 Table M-2 - FY 2004 Implementation Monitoring Selection Categories 81 Table M-3 - Comparison of Projected vs. Actual Harvest Volume (MMBF)/Acres to Date 82 Table M-4 - Timber Sale Volume and Acres Offered (Entire Resource Area) 83 Table M-5 - Timber Sale Monitoring Summary 89 Table M-6 - Post Treatment Stand Characteristics for West Grenada Timber Sale - FY 2004 90 Table M-7 - Status of Watershed Analysis 98 List of Figures Figure 1 - General Location Map 2 Figure 2 - KFRA Land Allocations 7 Xll Title: Annual program summary 2004 Author: United States. Bureau of Land Management. Klamath Falls Resource Area Office District Year: 2005 Annual Program Summary and Monitoring Report - FY2004 Table of Contents ANNUAL PROGRAM SUMMARY 1.0 Introduction 3 2.0 Summary of Accomplishments 3 3.0 Budget and Employment 6 4.0 Land Use Allocations within the Klamath Falls Resource Area 6 Late-Successional Reserves and Assessments 8 Matrix 8 5.0 Aquatic Conservation Strategy 9 Riparian Reserves 9 Watershed Analysis and Key Watersheds 9 Watershed Restoration 10 Roads 10 Riparian Habitat Enhancement 10 Stream Restoration 11 6.0 Air Quality 11 7.0 Water and Soils 11 Water - Project Implementation 11 Soils - Project Implementation 12 Water - Inventory and Monitoring 12 Soils -Inventory and Monitoring 13 State-listed Clean Water Act 303d Streams 13 RMP Best Management Practices 13 8.0 Terrestrial Species and Habitat Management 14 Survey and Manage Species 14 Threatened/Endangered Species 14 Northern Spotted Owl 14 Bald Eagle 14 Special Status Species-Animals 15 Peregrine Falcon 15 Yellow Rails 15 Bats 15 Northern Goshawk 15 Oregon Spotted Frog 15 Sage Grouse 16 vii Klamath Falls Resource Area Mollusks 16 Great Gray Owl 16 Special Status Species - Plants 16 Other Species of Concern 17 Neotropical Migratory Landbirds 17 Terrestrial Habitat Management 17 Nest Sites, Activity Centers, and Rookeries 17 Big Game Habitat 19 9.0 Aquatic Species and Habitat Management 19 Threatened/Endangered Species 19 Lost River and Shortnose Suckers 19 Bull Trout 20 Endangered Species Act Consultation 20 Aquatic Habitat Restoration 20 Klamath River Hydroelectric Facility Relicensing 21 10.0 Pathogen, Disease, and Pest Management 21 11.0 Weed Management 22 Inventories 22 Control 22 12.0 Special Areas/Management 23 Wild and Scenic Rivers 23 Wilderness 23 Areas of Critical Environmental Concern 23 Tunnel Creek Special Botanical Area 24 Klamath Canyon ACEC 24 Old Baldy Research Natural Area 24 Wood River Wetland ACEC 24 Environmental Education Areas 25 13.0 Cultural Resources 26 14.0 Visual Resources 26 15.0 Rural Interface Areas 26 16.0 Socioeconomic Conditions 27 Jobs-in-the-Woods 28 17.0 Environmental Justice 30 18.0 Recreation 30 Recreation Pipeline Restoration Funds 30 Recreation Projects 31 viii Annual Program Summary and Monitoring Report - FY2004 Recreation Fee Demonstration Project 31 Status of Recreation Plans 32 Volunteer Activities 32 Tourism 33 19.0 Forest Management and Timber Resources 33 Silvicultural Prescriptions 33 Timber Sale Planning 34 FY 2004 Timber Sale Accomplishments 34 Status of Sold & Awarded Klamath Falls RMP Timber Sales 35 Forest Development Activities 39 Stewardship Contracting 42 20.0 Special Forest Products 42 21.0 Energy and Minerals 43 22.0 Land Tenure Adjustments 44 23.0 Access and Rights-of-Way 45 24.0 Transportation and Roads 45 25.0 Hazardous Materials 46 26.0 Wildfire/Fuels Management 46 27.0 Law Enforcement 47 28.0 Rangeland Resources / Grazing Management 48 Fiscal Year 2004 Summary 49 Fiscal Years 1996-2004 Summary 50 Wild Horse Management 51 29.0 Cadastral Survey 52 30.0 Education and Outreach 52 31.0 Research 56 32.0 Coordination and Consultation 58 Federal Agencies 58 State of Oregon 58 Counties 59 Cities 59 Tribes 59 IX Klamath Falls Resource Area Watershed Councils 59 Chartered Advisory Groups 60 Other Local Coordination and Cooperation 61 33.0 National Environmental Policy Act Analysis and Documentation 63 NEPA documentation 63 Klamath Falls Resource Area Environmental Documentation 63 Protests and Appeals 63 34.0 Plan Evaluations 64 Third Year Evaluation 64 Eighth Year Evaluation 64 35.0 Plan Maintenance 65 36.0 Plan Amendments 72 Plan Revision 76 MONITORING REPORT Introduction 79 All Land Use Allocations 83 Late-Successional Reserves 86 Matrix 88 Riparian Reserves 92 Air Quality 95 Water and Soils 96 Terrestrial Species Habitat 101 Special Status and SEIS Special Attention Species Habitat 106 Aquatic Species Habitat 110 Noxious Weeds 112 Special Areas 113 Wild and Scenic Rivers 115 Cultural Resources Including American Indian Values 116 Visual Resources 118 Rural Interface Areas 119 Socioeconomic Conditions 120 Recreation 121 Forest Management and Timber Resources 121 Special Forest/Natural Products 122 Wildfire / Fuels Management 124 Rangeland Resources / Grazing Management 124 GLOSSARY/ACRONYMS 129 Annual Program Summary and Monitoring Report - FY2004 List of Tables Table 2.1 - Summary of Resource Management Actions, Directions, and Accomplishments 4 Table 2.1 - Summary of Resource Management Actions, Directions, and Accomplishments (Cont.).5 Table 3.1 - Resource Area Budget Fiscal Year 2004 6 Table 4.1 - Land Use Allocation 8 Table 5.1 - Watershed Analysis Schedule 10 Table 5.2-Watershed Analysis Status Fiscal Year 2004 10 Table 6.1 -Air Quality Management Fiscal Year 2004 11 Table 7.1 - Watershed Activity Fiscal Year 2004 12 Table 7.2 - KFRA Clean Water Act 303(d) Water Bodies 13 Table 8.1a - BLM /KFRA Special Status Species Designations Summary -Animals 18 Table 8.1b - BLM (KFRA) Special Status Species Designations Summary - Plants 18 Table 8.2 - Terrestrial Habitat Monitoring Fiscal Year 2004 18 Table 8.3 - Monitoring for Nest Sites, Activity Centers, Rookeries, Special Habitats 18 Table 9.1 -Aquatic Habitat/ Fish Passage Management Fiscal Year 2004 19 Table 11.1 - Managed Weed Species 20 Table 12.1 - Special Management Areas 25 Table 13.1 - Cultural Resources Management Fiscal Year 2004 26 Table 16.1 - Total Payments in Lieu of Taxes and Acres by County for FY 2004 28 Table 16.2 - O&C Payments To Counties FY 2004 29 Table 16.3 - Jobs in the Woods Program Fiscal Year 2004 29 Table 18.1 - Recreation Statistics Fiscal Year 2004 30 Table 18.2 - Recreation Fee Demonstration Project Fiscal Year 2004 32 Table 19.1 - Klamath Falls Timber Sale Volume (MBF) and Acres FY 2004 35 Table 19.2-Timber Volume Sold in FY 2004 36 Table 19.3 - Harvest Activity for FY 2004 36 Table 19.4 - Planned Timber Sales (FY 2005 & 2006) 36 Table 19.5 - Status of Sold and Awarded Timber Sales 37 Table 19.6 - Summary of Volume Sold 38 Table 19.7 -Volume and Acres Sold by Allocations 38 Table 19.8 - Timber Sales Sold by Harvest Types 38 Table 19.9 - Timber Sale Acres Sold by Age Class 39 Table 19.10 - Forest Development Activities 41 Table 20.1 - Special Forest Products Fiscal Year 2004 43 Table 21.1 - Energy and Minerals Management Fiscal Year 2004 44 Table 22.1 - Land Use Tenure Adjustments Fiscal Year 2004 45 Table 24.1 - Roads and Transportation Management Fiscal Year 2004 45 Table 25.1 - Hazardous Materials Management Fiscal Year 2004 46 Table 26.1 - Fire and Fuels Management Fiscal Year 2004 46 Table 27.1 - Law Enforcement Fiscal Year 2004 47 Table 28.1 - Range Resources Management Fiscal Year 2004 48 Table 29.1 -Cadastral Survey Summary Fiscal Year 2004 52 Table 30.1 - Environmental Education/Outreach Program Summary FY2004 54 Table 30.2 - Environmental Education/Outreach Special Events FY2004 55 Table 30.3 - Environmental Education/Outreach Programs & Tours FY 2004 56 Table 32.1 - Challenge Cost Share Fiscal Year 2004 62 XI Klamath Falls Resource Area Table 33.1 - NEPA Analyses and Documentation Fiscal Year 2004 64 Table 36.1 - Redefined Survey and Manage Categories 74 Table M.I - Projects Monitored FY 2004 80 Table M-2 - FY 2004 Implementation Monitoring Selection Categories 81 Table M-3 - Comparison of Projected vs. Actual Harvest Volume (MMBF)/Acres to Date 82 Table M-4 - Timber Sale Volume and Acres Offered (Entire Resource Area) 83 Table M-5 - Timber Sale Monitoring Summary 89 Table M-6 - Post Treatment Stand Characteristics for West Grenada Timber Sale - FY 2004 90 Table M-7 - Status of Watershed Analysis 98 List of Figures Figure 1 - General Location Map 2 Figure 2 - KFRA Land Allocations 7 Xll Close

• 3187. [Image] Farming practices and water quality in the Upper Klamath Basin : final report to the California State Water Resources Control Board : 205j program

  	Summary The Upper Klamath Basin (UKB) is a high desert region straddling the California-Oregon border east of the Cascade Range. Irrigation and other agricultural practices in the U. S. Bureau of Reclamation's ...
  	Citation × Citation Citation Abstract Copy Title: Farming practices and water quality in the Upper Klamath Basin : final report to the California State Water Resources Control Board : 205j program Author: Danosky, Earl; Kaffka, Stephen Year: 2002, 2007, 2006 Summary The Upper Klamath Basin (UKB) is a high desert region straddling the California-Oregon border east of the Cascade Range. Irrigation and other agricultural practices in the U. S. Bureau of Reclamation's Klamath Project may result in impaired surface water quality, reducing its use for wildlife and fish in important national wildlife refuges that receive drainage water from farms, and in the Klamath River. By 2004, a system of total maximum daily loads (TMDL) for nutrients must be established for the Klamath River. To investigate the relationships among agricultural practices and surface water quality in the Upper Klamath Basin, a two year reconnaissance survey of surface water and agricultural tile drain locations, focusing on nitrogen and phosphorus concentrations and mass transfers was conducted. Data was collected at 18 surface locations and 10 tile drain locations. Triplicate samples were taken every ten days during the growing season (April through October) and one or two times a month during the remainder of the months, depending on opportunity. No samples were taken from tile drains during the winter months because there was no irrigation and drainage during that period. Water samples were analyzed for phosphorus (total P, soluble reactive P, total filterable P, and particulate P) and nitrogen (total N, soluble N, Soluble organic N, total filterable N, particulate N, and ammonia N), temperature, pH and electrical conductivity, a measure of salinity or total dissolved solids. Analyses of data, including data quality, estimates of the transfer of nutrients in surface waters in the region, and hypotheses about the relationship between agriculture and water quality are reported. 1. The salt and nutrient content of surface waters increases nearly threefold as water moves through the watershed from the Lost River and J canal diversion to the Klamath Straits Drain. Mean ECW levels in input waters at the J canal diversion were approximately 250 \iS cm1, while water sampled at the D pump increased to 600 ^S cm"1 on average over the sample period. By the time water reenters the Klamath River, salt concentrations have increased to approximately 700 jaS cm1. 2. The ECW values observed in subsurface tile drains were higher on average than in input waters and surface waters elsewhere in the region, especially in the Lease Lands area of the Tulelake Irrigation District (TID). ECW values averaged approximately 2,500 ^S cm"1 . Recycling irrigation water through soils in the TID increases the salinity of the water, especially by the time it reaches and is reused in the Lease Lands area of the Tulelake National Wildlife Refuge (TLNWR). Soils in this part of the Klamath Project area are naturally high in salt. 3. Water temperatures in agricultural subsurface tile drains were significantly lower than surface water temperatures during the growing season when tile drains were active. pH values in tile drains were lower than surface water values. The temperature and pH of tile drains does not influence surface water values. 1. 4. For total phosphorus (TP) input waters at the J canal irrigation diversion for the TED averaged approximately 0.27 mg L1 for the two years reported. Water leaving the Tulelake Sumps at the D pump increases to 0.33 mg L1. Water leaving the Lower Klamath National Wildlife Refuge (LKNWR) sampled at the start of the Klamath Straits Drain, averaged 0.33 mg L1, similar to those at the D pump. TP increased further to 0.40 mg L"1 a the end of the Klamath Straits Drain. The overall increase in P concentration in surface waters was much less than for salt, suggesting that processes other than simple enrichment are occurring, particularly those associated with the exchange of sedimentary P and aquatic plant species. TN increases from 2.3 mg L"1 to 4.0 mg L1 over the same pathway. Atomic ratios (TN:TP) of surface water samples remain constant at approximately 10:1 throughout the system, suggesting that the amount of sediment and other small particulate matter in surface waters affects the values observed. The amount of sediment is influenced in part by the agitation of surface water as it passes through pumps and over weirs. 5. The average seasonal TP value in tile drains beneath farm fields is approximately 0.34 mg L"1 . While average total P values in subsurface tile drains were not different from those found at the D pump and the LKNWR outlet, the range in values was great (0.1 to 0.8 mg L1). Similarly, high NO3 -N values were observed at times in tile drains. Very high values in tile drains lead to the inference that some fertilizer N and P is lost in drainage water, combined with nutrients derived from decaying soil organic matter. The amount estimated as lost is much less than the amount of surplus fertilizer P applied and the amount of P surmised to be mineralized from decaying soil organic matter. P from fertilizer and decaying organic matter appears to be accumulating in soils and lake sediments in the region. 6. Ammonia N concentrations are at or below the limit of detection in subsurface agricultural tile lines and one to two orders of magnitude below the values observed in surface soils. Un ionized ammonia increases with temperature. Values above 0.25 mg L1 were observed in late summer at several locations. 7. Some leaching of soluble salts and nutrients is unavoidable when crops are irrigated. P fertilizer is applied at rates higher than crop removal, while fertilizer n is applied at rates less than crop removal. Reduced fertilizer use can help bring P inputs and outputs into balance and may reduce further any avoidable losses of P. This objective should be the subject of an agronomic research program in the region. 8. Surface waters entering the TDD, the TLNWR, and the LKNWR are already enriched with N and P. It seems unlikely that reducing N and P losses from farming in the TID, if possible, would influence surface water quality sufficiently to make them significantly less eutrophic. For P, the hypothesized threshold concentration limiting algae growth in fresh waters is 5 to 25 times smaller than the values observed in waters entering the TID for irrigation use. The addition of 1. nutrients from agriculture probably does not influence significantly surface water quality in the region. Wetland sediments, large amounts of organic matter in soils, and water introduced for irrigation contain essentially unlimited amounts of nutrients for aquatic plant growth. It is not clear how this circumstance could be changed under any reasonable time frame, if ever. 9. Using a TMDL approach may not result in reduced amounts of nutrients returned to the Klamath River because wetlands and farming practices in the southern portion of the Klamath Project result in the net removal of nutrients from the waters diverted for irrigation on a yearly basis, compared to allowing the same amount of water simply to flow down the river unused. Because of large errors of estimation for the amounts of water transferred, combined with smaller errors associated with estimating nutrient concentrations in water samples, and with year to year climate variation, TMDLs may not be an effective or efficient means of reducing nutrients in return flows to the Klamath River. Rational confidence limits for TMDLs may have to be too broad to be effective. Recycling of some drainage water for irrigation would reduce the amount of nutrients returned to the river more effectively than implementing a TMDL program. Title: Farming practices and water quality in the Upper Klamath Basin : final report to the California State Water Resources Control Board : 205j program Author: Danosky, Earl; Kaffka, Stephen Year: 2002, 2007, 2006 Summary The Upper Klamath Basin (UKB) is a high desert region straddling the California-Oregon border east of the Cascade Range. Irrigation and other agricultural practices in the U. S. Bureau of Reclamation's Klamath Project may result in impaired surface water quality, reducing its use for wildlife and fish in important national wildlife refuges that receive drainage water from farms, and in the Klamath River. By 2004, a system of total maximum daily loads (TMDL) for nutrients must be established for the Klamath River. To investigate the relationships among agricultural practices and surface water quality in the Upper Klamath Basin, a two year reconnaissance survey of surface water and agricultural tile drain locations, focusing on nitrogen and phosphorus concentrations and mass transfers was conducted. Data was collected at 18 surface locations and 10 tile drain locations. Triplicate samples were taken every ten days during the growing season (April through October) and one or two times a month during the remainder of the months, depending on opportunity. No samples were taken from tile drains during the winter months because there was no irrigation and drainage during that period. Water samples were analyzed for phosphorus (total P, soluble reactive P, total filterable P, and particulate P) and nitrogen (total N, soluble N, Soluble organic N, total filterable N, particulate N, and ammonia N), temperature, pH and electrical conductivity, a measure of salinity or total dissolved solids. Analyses of data, including data quality, estimates of the transfer of nutrients in surface waters in the region, and hypotheses about the relationship between agriculture and water quality are reported. 1. The salt and nutrient content of surface waters increases nearly threefold as water moves through the watershed from the Lost River and J canal diversion to the Klamath Straits Drain. Mean ECW levels in input waters at the J canal diversion were approximately 250 \iS cm1, while water sampled at the D pump increased to 600 ^S cm"1 on average over the sample period. By the time water reenters the Klamath River, salt concentrations have increased to approximately 700 jaS cm1. 2. The ECW values observed in subsurface tile drains were higher on average than in input waters and surface waters elsewhere in the region, especially in the Lease Lands area of the Tulelake Irrigation District (TID). ECW values averaged approximately 2,500 ^S cm"1 . Recycling irrigation water through soils in the TID increases the salinity of the water, especially by the time it reaches and is reused in the Lease Lands area of the Tulelake National Wildlife Refuge (TLNWR). Soils in this part of the Klamath Project area are naturally high in salt. 3. Water temperatures in agricultural subsurface tile drains were significantly lower than surface water temperatures during the growing season when tile drains were active. pH values in tile drains were lower than surface water values. The temperature and pH of tile drains does not influence surface water values. 1. 4. For total phosphorus (TP) input waters at the J canal irrigation diversion for the TED averaged approximately 0.27 mg L1 for the two years reported. Water leaving the Tulelake Sumps at the D pump increases to 0.33 mg L1. Water leaving the Lower Klamath National Wildlife Refuge (LKNWR) sampled at the start of the Klamath Straits Drain, averaged 0.33 mg L1, similar to those at the D pump. TP increased further to 0.40 mg L"1 a the end of the Klamath Straits Drain. The overall increase in P concentration in surface waters was much less than for salt, suggesting that processes other than simple enrichment are occurring, particularly those associated with the exchange of sedimentary P and aquatic plant species. TN increases from 2.3 mg L"1 to 4.0 mg L1 over the same pathway. Atomic ratios (TN:TP) of surface water samples remain constant at approximately 10:1 throughout the system, suggesting that the amount of sediment and other small particulate matter in surface waters affects the values observed. The amount of sediment is influenced in part by the agitation of surface water as it passes through pumps and over weirs. 5. The average seasonal TP value in tile drains beneath farm fields is approximately 0.34 mg L"1 . While average total P values in subsurface tile drains were not different from those found at the D pump and the LKNWR outlet, the range in values was great (0.1 to 0.8 mg L1). Similarly, high NO3 -N values were observed at times in tile drains. Very high values in tile drains lead to the inference that some fertilizer N and P is lost in drainage water, combined with nutrients derived from decaying soil organic matter. The amount estimated as lost is much less than the amount of surplus fertilizer P applied and the amount of P surmised to be mineralized from decaying soil organic matter. P from fertilizer and decaying organic matter appears to be accumulating in soils and lake sediments in the region. 6. Ammonia N concentrations are at or below the limit of detection in subsurface agricultural tile lines and one to two orders of magnitude below the values observed in surface soils. Un ionized ammonia increases with temperature. Values above 0.25 mg L1 were observed in late summer at several locations. 7. Some leaching of soluble salts and nutrients is unavoidable when crops are irrigated. P fertilizer is applied at rates higher than crop removal, while fertilizer n is applied at rates less than crop removal. Reduced fertilizer use can help bring P inputs and outputs into balance and may reduce further any avoidable losses of P. This objective should be the subject of an agronomic research program in the region. 8. Surface waters entering the TDD, the TLNWR, and the LKNWR are already enriched with N and P. It seems unlikely that reducing N and P losses from farming in the TID, if possible, would influence surface water quality sufficiently to make them significantly less eutrophic. For P, the hypothesized threshold concentration limiting algae growth in fresh waters is 5 to 25 times smaller than the values observed in waters entering the TID for irrigation use. The addition of 1. nutrients from agriculture probably does not influence significantly surface water quality in the region. Wetland sediments, large amounts of organic matter in soils, and water introduced for irrigation contain essentially unlimited amounts of nutrients for aquatic plant growth. It is not clear how this circumstance could be changed under any reasonable time frame, if ever. 9. Using a TMDL approach may not result in reduced amounts of nutrients returned to the Klamath River because wetlands and farming practices in the southern portion of the Klamath Project result in the net removal of nutrients from the waters diverted for irrigation on a yearly basis, compared to allowing the same amount of water simply to flow down the river unused. Because of large errors of estimation for the amounts of water transferred, combined with smaller errors associated with estimating nutrient concentrations in water samples, and with year to year climate variation, TMDLs may not be an effective or efficient means of reducing nutrients in return flows to the Klamath River. Rational confidence limits for TMDLs may have to be too broad to be effective. Recycling of some drainage water for irrigation would reduce the amount of nutrients returned to the river more effectively than implementing a TMDL program. Close

• 3188. [Image] Chronic toxicity of low dissolved oxygen concentrations, elevated pH, and elevated ammonia concentrations to lost river suckers (deltistes luxatus), and swimming performance of lost river suckers at various temperatures.

  	The study examines two species of sucker,the shortnose sucker(chasmistes brevirostrix), and the Lost River sucker,(deltisties luxatus) that inhabit Upper Klamath Lake and the effects of chronic toxicity ...
  	Citation × Citation Citation Abstract Copy Title: Chronic toxicity of low dissolved oxygen concentrations, elevated pH, and elevated ammonia concentrations to lost river suckers (deltistes luxatus), and swimming performance of lost river suckers at various temperatures. Author: Meyer, Joseph S. Year: 2000, 2007, 2006 The study examines two species of sucker,the shortnose sucker(chasmistes brevirostrix), and the Lost River sucker,(deltisties luxatus) that inhabit Upper Klamath Lake and the effects of chronic toxicity and temperature changes. The study examines two species of sucker,the shortnose sucker(chasmistes brevirostrix), and the Lost River sucker,(deltisties luxatus) that inhabit Upper Klamath Lake and the effects of chronic toxicity and temperature changes. Title: Chronic toxicity of low dissolved oxygen concentrations, elevated pH, and elevated ammonia concentrations to lost river suckers (deltistes luxatus), and swimming performance of lost river suckers at various temperatures. Author: Meyer, Joseph S. Year: 2000, 2007, 2006 The study examines two species of sucker,the shortnose sucker(chasmistes brevirostrix), and the Lost River sucker,(deltisties luxatus) that inhabit Upper Klamath Lake and the effects of chronic toxicity and temperature changes. The study examines two species of sucker,the shortnose sucker(chasmistes brevirostrix), and the Lost River sucker,(deltisties luxatus) that inhabit Upper Klamath Lake and the effects of chronic toxicity and temperature changes. Close

• 3189. [Image] Surface water-supply of the United States. pt. 11. Pacific slope basins in California

  	Includes Klamath River Basin; Chiefly tables; Includes indexes; Prepared in cooperation with the states and other agencies
  	Citation × Citation Citation Abstract Copy Title: Surface water-supply of the United States. pt. 11. Pacific slope basins in California Author: U.S. Dept. of the Interior, Geological Survey Year: 1910, 2008, 2005 Includes Klamath River Basin; Chiefly tables; Includes indexes; Prepared in cooperation with the states and other agencies Title: Surface water-supply of the United States. pt. 11. Pacific slope basins in California Author: U.S. Dept. of the Interior, Geological Survey Year: 1910, 2008, 2005 Includes Klamath River Basin; Chiefly tables; Includes indexes; Prepared in cooperation with the states and other agencies Close