Ground-Water Hydrology of the Upper Klamath Basin, Oregon and ...

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viii Conversion Factors and Datums Conversion Factors Multiply By To obtain acre 0.004047 square kilometer (km 2 ) acre-foot (acre-ft) 1,233 cubic meter (m 3 ) acre-foot per year (acre-ft/yr) 1,233 cubic meter per year (m 3 /yr) cubic foot (ft 3 ) 0.02832 cubic meter (m 3 ) cubic foot per second (ft 3 /s) 0.02832 cubic meter per second (m 3 /s) cubic foot per second per mile [(ft 3 /s)/mi] 0.0176 cubic meter per second per kilometer [(m 3 /s)/km] foot (ft) 0.3048 meter (m) foot per day (ft/d) 0.3048 meter per day (m/d) foot per mile (ft/mi) 0.1894 meter per kilometer (m/km) foot squared per day (ft 2 /d) 0.09290 meter squared per day (m 2 /d) gallon (gal) 3.785 liter (L) gallon per day per foot [(gal/d)/ft] 0.01242 cubic meter per day per meter [(m 3 /d)/m] gallon per minute (gal/min) 0.06309 liter per second (L/s) inch (in.) 2.54 centimeter (cm) inch per year (in/yr) 25.4 millimeter per year (mm/yr) mile (mi) 1.609 kilometer (km) million gallons (Mgal) 3,785 cubic meter (m 3 ) million gallons per day (Mgal/d) 0.04381 cubic meter per second (m 3 /s) square foot (ft 2 ) 0.09290 square meter (m 2 ) square mile (mi 2 ) 2.590 square kilometer (km 2 ) Temperature in degrees Fahrenheit (°F) may be converted to degrees Celsius (°C) as follows: Datums °C = (°F-32)/1.8. Horizontal coordinate information is referenced to the North American Datum of 1927 (NAD 27). Vertical coordinate information is referenced to the National Geodetic Vertical Datum of 1929 (NGVD 29). In this report, “altitude” refers to the distance above the vertical datum. *Transmissivity: The standard unit for transmissivity is cubic foot per day per square foot times foot of aquifer thickness [(ft 3 /d)/ft 2 ]ft. In this report, the mathematically reduced form, foot squared per day (ft 2 /d), is used for convenience.
ix Location System The system used for locating wells and springs in this report is based on the rectangular system for subdivision of public land. The States of Oregon and California are divided into 36 squaremile townships numbered according to their location relative to an east-west baseline and a north-south meridian. In Oregon, the Willamette base line and meridian are used, and in California, the Mount Diablo baseline and meridian are used. The position of a township is given by its north-south “Township” position relative to the baseline and its east-west “Range” position relative to the meridian. Each township is divided into 36 sections approximately 1 square mile (640-acre) in area and numbered from 1 to 36. For example, a well designated as 36S/11E- 20DCA is located in Township 36 south, Range 11 east, section 20. The three letters following the section number (A,B,C, or D) correspond to the location within the section; the first letter identifies the quarter section (160 acres), the second letter identifies the quarter-quarter section (40 acres), and the third letter identifies the quarter-quarter-quarter section (10 acres). Thus, well 20DCA is located in the NE quarter of the SW quarter of the SE quarter of section 20. When more than one designated well occurs in the quarter-quarter-quarter section, a serial number is appended. For some wells that were field located during previous studies or by the California Department of Water Resources, a different system of letters following the section number was used for the location within the section. This system assigns a letter to one of 16 quarter-quarter sections (40 acres) that divide the section. The location 20DCA corresponds to the location 20Q. When more than one designated well occurs in the quarter-quarter section, a serial number is appended. R. 8 E. R. 10 E. R. 12 E. R. 14 E. T. 34 S. T. 36 S. 6 5 4 3 2 1 7 8 9 10 11 12 18 17 16 15 14 13 19 20 21 22 23 24 30 29 28 27 26 25 31 32 33 34 35 36 B 20 A D E C F B G 20 A H C B D B A C C D A D M N L P K Q J R 36S/11E-20DCA 36S/11E-20Q
Page 1 and 2: Prepared in cooperation with the Or
Page 3 and 4: Ground-Water Hydrology of the Upper
Page 5 and 6: iii Contents Abstract..............
Page 7 and 8: Figures Figure 1. Map showing the u
Page 9: vii Figures—Continued Figure 30.
Page 13 and 14: Ground-Water Hydrology of the Upper
Page 15 and 16: Creek Introduction 43°15' 43°00'
Page 17 and 18: Introduction MEAN MONTHLY PRECIPIT
Page 19 and 20: Introduction 122°00' 45' 30' 121
Page 21 and 22: Geologic Framework basins separate
Page 23 and 24: Creek Creek Geologic Framework 11 4
Page 25 and 26: Geologic Framework 13 Hydraulic con
Page 27 and 28: Geologic Framework 15 Table 2. Summ
Page 29 and 30: Ground-Water Hydrology 17 100 90 80
Page 31 and 32: Ground-Water Hydrology 19 The sourc
Page 33 and 34: Ground-Water Hydrology 21 determine
Page 35 and 36: Ground-Water Hydrology 23 Geographi
Page 37 and 38: Ground-Water Hydrology 25 TOTAL WAT
Page 39 and 40: Ground-Water Hydrology 27 DISCHARGE
Page 41 and 42: Ground-Water Hydrology 29 SEPTEMBER
Page 43 and 44: Ground-Water Hydrology 31 Upper Kla
Page 45 and 46: Ground-Water Hydrology 33 The Lost
Page 47 and 48: Ground-Water Hydrology 35 Most grou
Page 49 and 50: Ground-Water Hydrology 37 INFLOW, I
Page 51 and 52: Ground-Water Hydrology 39 example,
Page 53 and 54: Ground-Water Hydrology 41 Recent In
Page 55 and 56: Ground-Water Hydrology 43 122°00'
Page 57 and 58: Creek Ground-Water Hydrology 45 43
Page 59 and 60: Ground-Water Hydrology 47 5 ft/mi.
Page 61 and 62:
Creek Ground-Water Hydrology 49 43
Page 63 and 64:
Ground-Water Hydrology 51 DEPTH TO
Page 65 and 66:
Ground-Water Hydrology 53 35 37 Dep
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Ground-Water Hydrology 55 4144 4143
Page 69 and 70:
Ground-Water Hydrology 57 Water lev
Page 71 and 72:
Ground-Water Hydrology 59 Long-term
Page 73 and 74:
Ground-Water Hydrology 61 122°00'
Page 75 and 76:
Ground-Water Hydrology 63 122°00'
Page 77 and 78:
Acknowledgments 65 Hydraulic head i
Page 79 and 80:
References Cited 67 Cooper, R.M., 2
Page 81 and 82:
References Cited 69 Theis, C.V., 19
Page 83 and 84:
Appendix A. 71 Appendix A. Landsat
Page 85 and 86:
Table 6 73 Table 6. Estimated groun
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Manuscript approved for publication
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Ground-Water Hydrology of the Upper Klamath Basin, Oregon and ...

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