Hydrology of Bishop Creek, Inyo County, California: an Isotopic Analysis
Total Page:16
File Type:pdf, Size:1020Kb
UNLV Retrospective Theses & Dissertations 1-1-1988 Hydrology of Bishop Creek, Inyo County, California: An isotopic analysis Michael Louis Space University of Nevada, Las Vegas Follow this and additional works at: https://digitalscholarship.unlv.edu/rtds Repository Citation Space, Michael Louis, "Hydrology of Bishop Creek, Inyo County, California: An isotopic analysis" (1988). UNLV Retrospective Theses & Dissertations. 18. http://dx.doi.org/10.25669/hhdn-m2k0 This Thesis is protected by copyright and/or related rights. It has been brought to you by Digital Scholarship@UNLV with permission from the rights-holder(s). You are free to use this Thesis in any way that is permitted by the copyright and related rights legislation that applies to your use. For other uses you need to obtain permission from the rights-holder(s) directly, unless additional rights are indicated by a Creative Commons license in the record and/ or on the work itself. This Thesis has been accepted for inclusion in UNLV Retrospective Theses & Dissertations by an authorized administrator of Digital Scholarship@UNLV. For more information, please contact [email protected]. INFORMATION TO USERS The most advanced technology has been used to photo graph and reproduce this manuscript from the microfilm master. UMI films the text directly from the original or copy submitted. Thus, some thesis and dissertation copies are in typewriter face, while others may be from any type of computer printer. The quality of this reproduction is dependent upon the quality of the copy submitted. Broken or indistinct print, colored or poor quality illustrations and photographs, print bleedthrough, substandard margins, and improper alignment can adversely affect reproduction. In the unlikely event that the author did not send UMI a complete manuscript and there are missing pages, these will be noted. Also, if unauthorized copyright material had to be removed, a note will indicate the deletion. Oversize materials (e.g., maps, drawings, charts) are re produced by sectioning the original, beginning at the upper left-hand corner and continuing from left to right in equal sections with small overlaps. Each original is also photographed in one exposure and is included in reduced form at the back of the book. These are also available as one exposure on a standard 35mm slide or as a 17" x 23" black and white photographic print for an additional charge. Photographs included in the original manuscript have been reproduced xerographically in this copy. Higher quality 6" x 9" black and white photographic prints are available for any photographs or illustrations appearing in this copy for an additional charge. Contact UMI directly to order. University Microfilms International A Bell & Howell Information Company 300 North Zeeb Road, Ann Arbor, Ml 48106-1346 USA 313/761-4700 800/521-0600 Order Number 1337598 Hydrology of Bishop Creek, Inyo County, California: An isotopic analysis Space, Michael Louis, M.S. University of Nevada, Las Vegas, 1989 UMI 300 N. Zeeb Rd. Ann Arbor, MI 48106 Hydrology of Bishop Creek, Inyo County, California: An Isotopic Analysis by Michael Louis Space A thesis submitted in partial fulfillment of the requirements for the degree of Master of Science in Geoscience Department of Geoscience University of Nevada, Las Vegas May 1989 The thesis of Michael Louis Space for the degree of Master of Science Geoscience is approved. Chairman, John W. Hess, Ph.D. <rr\ _ Examining Committee MencLhef, Stephen A. Mizell, Ph.D / / Examining Committee Member, David L. Weide, Ph.D. Graduate Faculty Representative, Stanley D. Smith, Ph.D. Graduate Dean, Ronald W. Smith, Ph.D. University of Nevada, Las Vegas May 1989 ABSTRACT Bishop Creek, located in east-central California on the eastern side of the Sierra Nevada supports fauna and flora that otherwise could not exist. There are approximately 3000 meters of relief in the Bishop Creek watershed. The headwaters of the creek originate from three man-made lakes, situated at 2790 to 2975 meters above sea level. During its course, diverted water from Bishop Creek flows through a series of five hydroelectric power plants, resulting in streamflow that is less than that expected under natural conditions much of the year. Stream diversion for hydroelectric power production may have adverse effects on the riparian community. An isotopic study was employed to better understand the hydrology of the basin, estimate the volume of ground-water input along diverted reaches of Bishop Creek, and determine the sources of water to different tree species at various times of the growing season. Sampling of both fresh and integrated snow during January and April, 1988 show relative enrichments in both and <5D values in snow for April. This was primarily due to the removal of isotopically lighter snow during melting periods and an influx of isotopically heavier snow during the warmer spring months. The average <5D value of the snowpack sampled for April 1988 is -158 °/oo. Tributary waters that flow into the headwater lakes of Bishop Creek have an average 5D value of -131 °/oo for April 1988. Ground water sampled from the Bishop Creek basin during 1986-1987 have an average 5D value of -133 °/oo. From interpretation of the isotope data it was concluded that snowmelt infiltrated the ground surface and displaced ground water into the tributary streams. Summer precipitation 8 D values collected in 1988 have an unweighted average of -67 °/oo. An isotopic balance provides a rough estimate that 75% of the ground water is from winter precipitation in the basin. Bishop Creek was divided into 7 reaches and ground-water discharge was estimated using an isotopic-mass balance equation. Average 8 D values of lake headwaters are 10-15 °/oo more enriched relative to ground-water 8 D values. Iso topic shifts to more negative 8 D values along Bishop Creek occurred during low flow conditions for 1986-1987. This was especially true for reaches found at higher elevations. Isotopic shifts were not detected during high streamflow periods because ground-water input was insignificant to surface water flow. In July and October, 1987, diverted reaches showed a range of ground-water input from zero to 0.054 m3/s. Total flow through the gaining reaches varied from 0.018 to 0.135 m3/s. The 8 D values for various tree species along the riparian corridor and on a hillslope above the stream were, on the average, more depleted than possible water sources. Testing of the laboratory method of cottonwood trees along a wash in Southern Nevada showed that this was partly due to the length of the distillation time of the tree sample. However, variations in the 8 D values of the tree samples along the wash varied by as much as 14 °/oo. This was probably a result of either biological fractionation of the water by the plant or differences in water source. TABLE OF CONTENTS ABSTRACT ........................................................................................................................ ill LIST OF FIGURES .......................................................................................................... vi LIST OF TABLES.............................................................................................................viii ACKNOWLEDGEMENTS............................................................................................. ix INTRODUCTION .............................................................................................................. 1 O bjectives ......................................................................................................................... 2 Previous Studies ............................................................................................................. 3 ENVIRONMENTAL SETTING .....................................................................................5 G eography ........................................................................................................................ 5 Hydroelectric Power Production On Bishop Creek ............................................. 5 Climate and Vegetation ................................................................................................7 Precipitation Data for Bishop Creek, 1985-1987 .................................................. 10 G eology ............................................................................................................................. 12 L ithology ......................................................................................................................12 Tectonic History ........................................................................................................ 14 Local Hydrogeology ....................................................................................................... 15 STABLE ENVIRONMENTAL ISOTOPES ...............................................................18 Introduction .................................................................................................................... 18 Stable Isotopes in the Hydrologic Cycle .................................................................20 Stable Isotopes in Trees ................................................................................................22 METHODS AND PROCEDURES................................................................................25 Field Methods .................................................................................................................. 25 Surface