Update of 1982 Six State High Plains Aquifer Study
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Assessing the Potential of Reservoir Outflow Management to Reduce
HYDROLOGICAL PROCESSES Hydrol. Process. 27, 1426–1439 (2013) Published online 23 April 2012 in Wiley Online Library (wileyonlinelibrary.com) DOI: 10.1002/hyp.9284 Assessing the potential of reservoir outflow management to reduce sedimentation using continuous turbidity monitoring and reservoir modelling† Casey Lee* and Guy Foster US Geological Survey, Lawrence, KS, 66049, USA Abstract: In-stream sensors are increasingly deployed as part of ambient water quality-monitoring networks. Temporally dense data from these networks can be used to better understand the transport of constituents through streams, lakes or reservoirs. Data from existing, continuously recording in-stream flow and water quality monitoring stations were coupled with the two-dimensional hydrodynamic CE-QUAL-W2 model to assess the potential of altered reservoir outflow management to reduce sediment trapping in John Redmond Reservoir, located in east-central Kansas. Monitoring stations upstream and downstream from the reservoir were used to estimate 5.6 million metric tons of sediment transported to John Redmond Reservoir from 2007 through 2010, 88% of which was trapped within the reservoir. The two-dimensional model was used to estimate the residence time of 55 equal- volume releases from the reservoir; sediment trapping for these releases varied from 48% to 97%. Smaller trapping efficiencies were observed when the reservoir was maintained near the normal operating capacity (relative to higher flood pool levels) and when average residence times were relatively short. An idealized, alternative outflow management scenario was constructed, which minimized reservoir elevations and the length of time water was in the reservoir, while continuing to meet downstream flood control end points identified in the reservoir water control manual. -
Kansas Resource Management Plan and Record of Decision
United States Department of the Interior Bureau of Land Management Tulsa District Oklahoma Resource Area September 1991 KANSAS RESOURCE MANAGEMENT PLAN Dear Reader: This doCument contains the combined Kansas Record of Decision (ROD) and Resource Management Plan (RMP). The ROD and RMP are combined to streamline our mandated land-use-planning requirements and to provide the reader with a useable finished product. The ROD records the decisions of the Bureau of Land Management (BLM) for administration of approximately 744,000 acres of Federal mineral estate within the Kansas Planning Area. The Planning Area encompasses BLM adm in i sterad sp 1 it-estate mi nera 1 s and Federa 1 minerals under Federal surface administered by other Federal Agencies within the State of Kansas. The Kansas RMP and appendices provide direction and guidance to BLM Managers in the formulation of decisions effecting the management of Federal mineral estate within the planning area for the next 15 years. The Kansas RMP was extracted from the Proposed Kansas RMP/FIES. The issuance of this ROD and RMP completes the BLM land use planning process for the State of Kansas. We now move to implementation of the plan. We wish to thank all the individuals and groups who participated in this effort these past two years, without their help we could not have completed this process. er~ 1_' Area Manager Oklahoma Resource Area RECORD OF DECISION on the Proposed Kansas Resource Management Plan and Final Environmental Impact Statement September 1991 RECORD OF DECISION The decision is hereby made to approve the proposed decision as described in the Proposed Kansas Resource Management Plan/Final Env ironmental Impact Statement (RMP/FEIS July 1991), MANAGEMENT CONSZOERATXONS The decision to approve the Proposed Plan is based on: (1) the input received from the public, other Federal and state agencies; (2) the environmental analysis for the alternatives considered in the Draft RMP/Oraft EIS, as we11 as the Proposed Kansas RMP/FEIS. -
Characterization of Surface-Water
U.S. Department of the Interior U.S. Geological Survey Characterization of Surface-Water Quality Based on Real-Time Monitoring and Regression Analysis, Quivira National Wildlife Refuge, South-Central Kansas, December 1998 Through June 2001 By VICTORIA G. CHRISTENSEN Water-Resources Investigations Report 01–4248 Prepared in cooperation with the U.S. FISH AND WILDLIFE SERVICE Lawrence, Kansas 2001 U.S. Department of the Interior Gale A. Norton, Secretary U.S. Geological Survey Charles G. Groat, Director For additional information write to: Copies of this report can be purchased from: U.S. Geological Survey District Chief Information Services U.S. Geological Survey Building 810, Federal Center 4821 Quail Crest Place Box 25286 Lawrence, KS 66049–3839 Denver, CO 80225–0286 CONTENTS Abstract.................................................................................................................................................................................. 1 Introduction ........................................................................................................................................................................... 2 Purpose and Scope....................................................................................................................................................... 4 Description of Study Area ........................................................................................................................................... 4 Methods ................................................................................................................................................................................ -
Little Arkansas River Crossing Other Names/Site Number KHRI #159-113; Archeological Site #14RC1302; NPS Plan #87
NPS Form 10-900 0MB No. 1024-0018 United States Department of the Interior 17ECEIVED 2280 National Park Service _ FEB 18 2014 National Register of Historic Places i'.lFGI STER OF HISTORIC PLACES Registration Form 1~:c\l l! ll\l.i\L PA RK SERVICE This form is for use in nominating or requesting determinations for individual properties and districts. See instructions in National Register Bulletin, How to Complete the National Register of Historic Places Registration Form. If any item does not apply to the property being documented, enter "N/A" for "not applicable." For functions, architectural classification, materials, and areas of significance, enter only categories and subcategories from the instructions. Place additional certification comments, entries, and narrative items on continuation sheets if needed (NPS Form 10- 900a). 1. Name of Property historic name Little Arkansas River Crossing other names/site number KHRI #159-113; Archeological site #14RC1302; NPS Plan #87 2. Location street & number NE intersection Ave P & 30th Rd D not for publication city or town __W_ in_d_o_m__ ____ ___________________ ~ vicinity state Kansas code KS county Rice code 159 zip code 67491 3. State/Federal Agency Certification As the designated authority under the National Historic Preservation Act, as amended, I hereby certify that this _x_ nomination_ request for determination of eligibility meets the documentation standards for registering properties in the National Register of Historic Places and meets the procedural and professional requirements set forth in 36 CFR Part 60. In my opinion, the property _x_ meets __ does not meet the National Register Criteria. I recommend that this property be considered significant at the following level(s) of significance: X national statewide - local ~ eJk~ DSJ-1£() 9.-1 /.·lt Signature of c~ ing official/Title Date State or Federal agency/bureau or Tribal Government In my opinion, the property _meets_ does not meet the National Register criteria. -
Streamflow Depletion Investigations in the Republican River Basin: Colorado, Nebraska, and Kansas
J. ENVIRONMENTAL SYSTEMS, Vol. 27(3) 251-263, 1999 STREAMFLOW DEPLETION INVESTIGATIONS IN THE REPUBLICAN RIVER BASIN: COLORADO, NEBRASKA, AND KANSAS JOZSEF SZILAGYI University of Nebraska–Lincoln ABSTRACT Water is a critical resource in the Great Plains. This study examines the changes in long-term mean annual streamflow in the Republican River basin. In the past decades this basin, shared by three states, Colorado, Nebraska, and Kansas, displayed decreased streamflow volumes as the river enters Kansas across the Nebraska-Kansas border compared to values preceding the 1950s. A recent lawsuit filed by Kansas challenges water appropriations in Nebraska. More than half of the source area for this water, however, lies outside of Nebraska. Today a higher percentage of the annual flow is generated within Nebraska (i.e., 75% of the observed mean annual stream- flow at the NE-KS border) than before the 1950s (i.e., 66% of the observed mean annual streamflow) indicating annual streamflow has decreased more dramatically outside of Nebraska than within the state in the past fifty years. INTRODUCTION The Republican River basin’s 64,796 km2 drainage area is shared by three states: Colorado, Nebraska, and Kansas (see Figure 1). Nebraska has the largest single share of the drainage area, 25,154 km2 (39% of total); Colorado can claim about 20,000 km2 (31%), while the rest, about 19,583 km2 (30%), belongs to Kansas [1], from which about 12,800 km2 (20%) lies upstream of Hardy, near the Nebraska-Kansas border. Exact figures for the contributing drainage areas (portions of the drainage areas that actually contribute water to the stream) are hard to obtain because these areas in the headwater sections of the basin have been shrinking constantly in the past fifty years. -
FLINT HILLS MTIONAL WILDLIFE REFUGE Hartford, Kansas
FLINT HILLS MTIONAL WILDLIFE REFUGE Hartford, Kansas ANNUAL NARRATIVE REPORT Calendar Year 1977 NATIONAL WILDLIFE REFUGE SYSTEM Pish and Wildlife Service U.S. DEPARTMENT OP THE INTERIOR yr^mr ETLI^ fatioml I Bartfocpd, Ktosaa AHSDJIL HAHRimrg hspght CaOondar Tear 1977 mmOML WIWUM BBPUQ3 STE™ Flah and Wildlife Servloe 0,3, 0^ THB UfffiHIOK Bsraciunol 1. Harold B. Sbdpbard Tractor Operator WG-06-433 (Career Ssasoml) 2. 7, Amdt Clerk Typist GS-03-02 (CC-PPT) 3* Carltoil IU Freoburg Asst. Bsfugs mmm* GS-09-01 (P?T) U. Hon £• Thum l&lntsnaras Worker WG~07-01 {CC-OT?) - Hot Pictured - Iltohael J. Long Mfvim Manager (^-11-02(m) Joseph L. PXusisr Bio, Iteoh. 03-05-03 (TT) Bsslgnsd 10/27/77 Joseph J. Conrad Traotor Operator WG-0&-03 (FT} Betired 10/18/77 Berioi# and As/fif} £u.i' Kotfo $J? 7// y Bats FLINT HILLS Flint Hills National Wildlife Refuge NATIONAL WILDLIFE REFUGE was established under the authority of the Fish and Wildlife Coordination Act on a part of the area acquired by the U.S. Army Corps of Engineers for the John Redmond Dam and Reservoir. This flood control project is administered by the District Engineer, Tulsa, Oklahoma. PUBLIC ROADS SPECIAL RECREATION AREAS - NO HUNTING STRAWN HUNTING AREA FISHING ACCESS POINTS (1) DESIGNATED FIREARM TRAVEL ROUTE (During waterfowl hunting season. TABLES OF CCMSSTS I* GgKBaAL 3&ge A. Introduotlon 1 B. dim tic and Habitat Ccaiditiona 1 C. Land Acquisition. 2 B. System Status • 2 n* ocmmxiTim MD mnmmim A. Conatruotion k B. Maintenance 6 C. Wildfire . -
Suspended-Sediment Loads, Reservoir Sediment Trap Efficiency, and Upstream and Downstream Channel Stability for Kanopolis and Tuttle Creek Lakes, Kansas, 2008–10
Prepared in cooperation with the Kansas Water Office Suspended-Sediment Loads, Reservoir Sediment Trap Efficiency, and Upstream and Downstream Channel Stability for Kanopolis and Tuttle Creek Lakes, Kansas, 2008–10 Scientific Investigations Report 2011–5187 U.S. Department of the Interior U.S. Geological Survey Front cover. Upper left: Tuttle Creek Lake upstream from highway 16 bridge, May 16, 2011 (photograph by Dirk Hargadine, USGS). Lower right: Tuttle Creek Lake downstream from highway 16 bridge, May 16, 2011 (photograph by Dirk Hargadine, USGS). Note: On May 16, 2011, the water-surface elevation for Tuttle Creek Lake was 1,075.1 feet. The normal elevation for the multi-purpose pool of the reservoir is 1,075.0 feet. Back cover. Water-quality monitor in Little Blue River near Barnes, Kansas. Note active channel-bank erosion at upper right (photograph by Bill Holladay, USGS). Suspended-Sediment Loads, Reservoir Sediment Trap Efficiency, and Upstream and Downstream Channel Stability for Kanopolis and Tuttle Creek Lakes, Kansas, 2008–10 By Kyle E. Juracek Prepared in cooperation with the Kansas Water Office Scientific Investigations Report 2011–5187 U.S. Department of the Interior U.S. Geological Survey U.S. Department of the Interior KEN SALAZAR, Secretary U.S. Geological Survey Marcia K. McNutt, Director U.S. Geological Survey, Reston, Virginia: 2011 For more information on the USGS—the Federal source for science about the Earth, its natural and living resources, natural hazards, and the environment, visit http://www.usgs.gov or call 1–888–ASK–USGS. For an overview of USGS information products, including maps, imagery, and publications, visit http://www.usgs.gov/pubprod To order this and other USGS information products, visit http://store.usgs.gov Any use of trade, product, or firm names is for descriptive purposes only and does not imply endorsement by the U.S. -
Kansas Department of Wildlife and Parks
Kansas Department of Wildlife, Parks, and Tourism Kansas Special Size Limits, Creel Limits, and Bait Restriction Tables Dated: July 1, 2018 Blue Catfish Creel Limits 5 fish daily creel limit Cheney Reservoir, Clinton Reservoir, El Dorado Reservoir, Elk City Reservoir, Glen Elder Reservoir, John Redmond Reservoir, Kanopolis Reservoir, LaCygne Reservoir, Lovewell Reservoir, Melvern Reservoir, Perry Reservoir, Pomona Reservoir, Tuttle Creek Reservoir, Wilson Reservoir Blue Catfish Length Limits 25 - 40 inch slot limit with no more than 1 fish 40-inch or larger. Blue Catfish between the lengths of twenty-five (25) and forty (40) inches are protected and must be returned to the water immediately when taken from the following waters: Milford Reservoir 25 - 35 inch slot limit with no more than 2 fish 35-inch or larger. Blue Catfish between the lengths of twenty-five (25) and thirty-five (35) inches are protected and must be returned to the water immediately when taken from the following waters: El Dorado Reservoir 35 inch minimum. Blue catfish of a length less than thirty-five (35) inches are protected and must be returned to the water immediately when taken from the following waters: Cheney Reservoir, Clinton Reservoir, Elk City Reservoir, Glen Elder Reservoir, Kanopolis Reservoir, Lovewell Reservoir, Melvern Reservoir, Perry Reservoir, Tuttle Creek Reservoir, Wilson Reservoir Channel Catfish Creel Limits 2 fish daily creel limit Andale-Renwick USD 267 Pond, Andover - Lake George, Arma City Lake, Atchison State Fishing Lake, Blue Mound City -
Republican River Valley and Adjacent Areas, Nebraska
A, Economic Geology, 97 B, Descriptive Geology 119 M, General Hydrograpmc investigations, 26 (0, Underground Waters, 72 DEPARTMENT OF THE INTERIOR UNITED STATES GEOLOGICAL SURVEY CHARLES I>. WALOOTT, DIKECTOR GEOLOGY AND WATER RESOURCES OF THE REPUBLICAN RIVER VALLEY AND ADJACENT AREAS, NEBRASKA G. E. CONDRA -FERTY OF -LOGICAL Sl'». WASHINGTON (GOVERNMENT PRINTING OFFICE 1907 CONTENTS. Page. Introduction __'___________________________________ 7 Geography _____________________________________ 8 Topography______________________.._ 8 Drainage _____________________________.____ 8 Climate "_________________________ _ _________ ._..__ 9 Temperature_______l_____________________ 9 Rainfall _____________________________________ 9 Winds_____________________________________ 10 Descriptive geology ________________________________ 10 General relations _____ _________ ___ ________ 10 Structure____________________________ 11 Description of the rocks____ ______________________ 11 Carboniferous system_______________________ 11 Cretaceous system.__________________________ 12 Dakota formation_________________________ 12 Character and thickness______________ 12 Distribution_________________ 13 Benton group________________________ 13 Members represented________________ 13 Graneros shale_ ________________________ 14 Character and thickness_________________ 14 Exposures,_________ _______ _-_________ 14 Greenhorn limestone_____________________ 14 Character and thickness___________________ 14 Fossils_________________________ 16 Carlile shale______.___________________ -
The Unionid Mollusks of the Upper Kansas Basin of Northwestern Kansas and Southwestern Nebraska
University of Nebraska - Lincoln DigitalCommons@University of Nebraska - Lincoln Transactions of the Nebraska Academy of Sciences and Affiliated Societies Nebraska Academy of Sciences 1997 The Unionid Mollusks of the Upper Kansas Basin of Northwestern Kansas and Southwestern Nebraska Ellet Hoke Follow this and additional works at: https://digitalcommons.unl.edu/tnas Part of the Life Sciences Commons Hoke, Ellet, "The Unionid Mollusks of the Upper Kansas Basin of Northwestern Kansas and Southwestern Nebraska" (1997). Transactions of the Nebraska Academy of Sciences and Affiliated Societies. 70. https://digitalcommons.unl.edu/tnas/70 This Article is brought to you for free and open access by the Nebraska Academy of Sciences at DigitalCommons@University of Nebraska - Lincoln. It has been accepted for inclusion in Transactions of the Nebraska Academy of Sciences and Affiliated Societiesy b an authorized administrator of DigitalCommons@University of Nebraska - Lincoln. 1997. Transactions of the Nebraska Academy of Sciences, 24: 35-62 THE UNIONID MOLLUSKS OF THE UPPER KANSAS BASIN OF NORTHWESTERN KANSAS AND SOUTHWESTERN NEBRASKA Ellet Hoke 1878 Ridgeview Circle Drive Manchester, Missouri 63021 ABSTRACT t t t A qualitative survey ofthe Upper Kansas Basin resulted Extending eastward from the plains of Colorado in the documentation of a unionid fauna consisting of twenty into southwestern Nebraska and northwestern Kan one native taxa, as well as the introduced bivalve Corbicula sas, the Upper Kansas Basin, as herein defined, encom fluminea. Biological diversity was greatest in the extreme 2 eastern portion of the basin with the highest concentrations passes an area of 116,195 km (Map 1). It may be occurring in the habitat-rich eastern-most creeks. -
Fluvial Sediment in the Little Arkansas River Basin Kansas
Fluvial Sediment in the Little Arkansas River Basin Kansas GEOLOGICAL SURVEY WATER-SUPPLY PAPER 1798-B Prepared in cooperation with the City of fflichita and the Kansas Water Resources Board Fluvial Sediment in the Little Arkansas River Basin Kansas By C. D. ALBERT and G. J. STRAMEL SEDIMENTATION IN SMALL DRAINAGE BASINS GEOLOGICAL SURVEY WATER-SUPPLY PAPER 1798-B Prepared in cooperation with the City of ff^ichita and the Kansas ff^ater Resources Board UNITED STATES GOVERNMENT PRINTING OFFICE, WASHINGTON : 1966 UNITED STATES DEPARTMENT OF THE INTERIOR STEWART L. UDALL, Secretary GEOLOGICAL SURVEY William T. Pecora, Director For sale by the Superintendent of Documents, U.S. Government Printing Office Washington, D.C. 20402 - Price 60 cents (paper cover) CONTENTS Page Abstract__._____________ ___________.__________________________ Bl Introduction._____________________________________________________ 1 Description of the basin.___________________________________________ 2 Geology. __________________________________________ 3 Geomorphology _ ______________________________________________ 4 Soils. ______________________________-_-_-__---___ 5 Land use and vegetation.______________________________________ 7 Climate._____________________________________________________ 7 Runoff ___________________________________________________ 8 Fluvial sediment._________________________________________________ 13 Field investigations and methods._______________________________ 13 Laboratory methods.__________________________________________ 14 Suspended sediment.__________________________________________ -
National Register Nomination
NPS Form 10-900 OMB No. 1024-0018 United States Department of the Interior National Park Service National Register Listed National Register of Historic Places June 23, 2016 Registration Form This form is for use in nominating or requesting determinations for individual properties and districts. See instructions in National Register Bulletin, How to Complete the National Register of Historic Places Registration Form. If any item does not apply to the property being documented, enter "N/A" for "not applicable." For functions, architectural classification, materials, and areas of significance, enter only categories and subcategories from the instructions. Place additional certification comments, entries, and narrative items on continuation sheets if needed (NPS Form 10-900a). 1. Name of Property Historic name Steele, Herbert & Eliza, House Other names/site number KHRI # 171-0000-00001 Name of related Multiple Property Listing N/A 2. Location Street & number West Scott Lake Drive (NE/4,SE/4,SW/4 S12-T16S-R33W) not for publication City or town Scott City X vicinity State Kansas Code KS County Scott Code 171 Zip code 67871 3. State/Federal Agency Certification As the designated authority under the National Historic Preservation Act, as amended, I hereby certify that this x nomination _ request for determination of eligibility meets the documentation standards for registering properties in the National Register of Historic Places and meets the procedural and professional requirements set forth in 36 CFR Part 60. In my opinion, the property x _ meets _ does not meet the National Register Criteria. I recommend that this property be considered significant at the following level(s) of significance: national statewide x local Applicable National Register Criteria: A x B x C ___D See file.