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1

Ontario. Ministry of Agriculture and Food. Water Source Heat Pumps. S.l: s.n, 1988.

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2

Ontario. Ministry of Agriculture and Food. Horticultural Uses of Water Source Heat Pumps. S.l: s.n, 1985.

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3

Sargeant, Debby. Fecal contamination source identification methods in surface water. [Olympia, Wash.]: Washington State Dept. of Ecology, 1999.

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4

American Society of Heating, Refrigerating and Air-Conditioning Engineers. Water-source heat pumps: Testing and rating for performance. Atlanta, GA: American Society of Heating, Refrigerating and Air-Conditioning Engineers, 1998.

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5

American Society of Heating, Refrigerating and Air-Conditioning Engineers. Water-source heat pumps: Testing and rating for performance. Atlanta, GA: American Society of Heating, Refrigerating and Air-Conditioning Engineers, 1998.

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6

Terrell, Charles R. Water quality indicators guide: Surface waters. Washington, D.C: U.S. Dept. of Agriculture, Soil Conservation Service, 1989.

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7

Patricia, Perfetti, and Terrene Institute, eds. Water quality indicators guide: Surface waters. 2nd ed. Washington, D.C: Terrene Institute, 1996.

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8

Terrell, Charles R. Water quality indicators guide: Surface waters. [Washington, D.C.]: U.S. Dept. of Agriculture, Soil Conservation Service, 1989.

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9

South Dakota. Dept. of Environment and Natural Resources. The 2010 South Dakota integrated report for surface water quality assessment. Pierre, S.D.]: South Dakota Dept. of Environment and Natural Resources, 2010.

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10

Chandler, Robert V. Evaluation of water-analysis data for surface-water sites in the Weeks Bay Watershed, Alabama: January 1994-September 1995. Tuscaloosa, Ala: Geological Survey of Alabama, Hydrogeology Division, 1998.

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11

Cheung, F. B. Critical heat flux (CHF) phenomenon on a downward facing curved surface: Effects of thermal insulation. Washington, DC: Division of Systems Technology, Office of Nuclear Regulatory Research, U.S. Nuclear Regulatory Commission, 1998.

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12

LeChevallier, Mark W. Short-term variability of Giardia cyst and Cryptosporidium oocyst concentrations in a surface water source used for potable water. Trenton, N.J: New Jersey Dept. of Environmental Protection, Division of Science and Research, 1998.

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13

Caldwell, Andral W. Determination of the primary and secondary source-water protection areas for selected surface-water public-supply systems in South Carolina, 1999. Columbia, S.C: U.S. Dept. of the Interior, U.S. Geological Survey, 2000.

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14

Caldwell, Andral W. Determination of the primary and secondary source-water protection areas for selected surface-water public-supply systems in South Carolina, 1999. Columbia, S.C: U.S. Dept. of the Interior, U.S. Geological Survey, 2000.

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15

Mitsch, William J. Reducing nutrient loads, especially nitrate-nitrogen, to surface water, groundwater, and the Gulf of Mexico: Topic 5, report for the integrated assessment on hypoxia in the Gulf of Mexico. Silver Spring, Md: U.S. Dept. of Commerce, National Oceanic and Atmospheric Administration, Coastal Ocean Program, 1999.

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16

Eddy-Miller, Cheryl A. Characterization of interactions between surface water and near-stream groundwater along Fish Creek, Teton County, Wyoming, by using heat as a tracer. Reston, Va: U.S. Geological Survey, 2009.

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17

Meyer, Kathleen R. Characterization of releases to surface water from the Rocky Flats Plant: Task 2, verification and analysis of source terms. Neeses, S.C: Radiological Assessments Corporation, 1999.

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18

Pennsylvania. Dept. of Environmental Protection. and Geological Survey (U.S.), eds. Use of stable isotopes of carbon, nitrogen, and sulfur to identify sources of nitrogen in surface waters in the lower Susquehanna River Basin, Pennsylvania. [Washington, D.C: U.S. G.P.O.], 2002.

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19

Cravotta, Charles A. Use of stable isotopes of carbon, nitrogen, and sulfur to identify sources of nitrogen in surface waters in the Lower Susquehanna River Basin, Pennsylvania. Lemoyne, Pa: U.S. Dept. of the Interior, U.S. Geological Survey ; Denver, Colo., 1995.

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20

Swain, Eric D. Development, testing, and application of a coupled hydrodynamic surface-water/groundwater model (FTLOADDS) with heat and salinity transport in the Ten Thousand Islands/Picayune Strand Restoration Project Area, Florida. Reston, Va: U.S. Dept. of the Interior, U.S. Geological Survey, 2009.

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21

Norton, Daniel R. Chloride flux and surface water discharge out of Yellowstone National Park, 1982-1989: Tabulation of discharge, chloride concentration, and chloride flux for the rivers and streams yields information related to heat flux from the park. Washington, D.C: U.S. G.P.O., 1991.

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22

Dexheimer, Donald R. Water Source Heat Pump Handbook. Natl Water Well Assn, 1985.

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23

Dexheimer, R. Water Source Heat Pump Handbook. Natl Water Well Assn, 1985.

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24

Washington (State). Division of Drinking Water., ed. Surface water as a source of public drinking water. [Olympia, Wash.]: Washington State Dept. of Health, Environmental Health Programs, Division of Drinking Water, 2003.

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25

Davisson, M. Lee. Isotopic Tracers in Surface Water. Amer Water Works Assn, 2002.

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26

Boyd, Matthew S. Heat source: Stream, river and open channel temperature prediction. 1996.

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27

United States. Environmental Protection Agency. Office of Water, ed. State methods for delineating source water protection areas for surface water supplied sources of drinking water. [Washington, D.C.]: U.S. Environmental Protection Agency, Office of Water, 1997.

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28

Aceves, Salvador M. Evaporator analysis for application to water-source and ice-maker heat pumps. 1989.

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29

Terrell, Charles R. Water Quality Indicators Guide: Surface Waters. Diane Pub Co, 1993.

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30

Water Quality Indicators Guide: Surface Waters. Diane Pub Co, 1991.

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31

United States. Environmental Protection Agency. Office of Ground-Water Protection, ed. A Review of methods for assessing nonpoint source contaminated ground-water discharge to surface water. [Washington, D.C.?]: Ground-Water Protection Division, U.S. Environmental Protection Agency, 1991.

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32

Yoon, Woon-young. Water quality effect on fouling of the heat transfer surface under forced circulation boiling condition. 1985.

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33

The 2006-2011 World Outlook for Ground and Ground Water Source Heat Pumps. Icon Group International, Inc., 2005.

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34

Parker, Philip M. The 2007-2012 World Outlook for Ground and Ground Water Source Heat Pumps. ICON Group International, Inc., 2006.

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35

Parker, Philip M. The 2007-2012 Outlook for Ground and Ground Water Source Heat Pumps in India. ICON Group International, Inc., 2006.

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36

Parker, Philip M. The 2007-2012 Outlook for Ground and Ground Water Source Heat Pumps in Japan. ICON Group International, Inc., 2006.

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37

V, Chandler Robert, and Geological Survey of Alabama. Hydrogeology Division., eds. Monitoring of surface-water and biological conditions in the Fish River Watershed of southwest Alabama: 1994. Tuscaloosa, Ala. (420 Hackberry Lane, P.O. Box O, Tuscaloosa 35486-9780): Geological Survey of Alabama, Hydrogeology Division, 1998.

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38

Authority, Tennessee Valley, ed. Water source heat pump: How to get home heating and cooling from your own back yard. [Knoxville, Tenn.?]: Tennessee Valley Authority, 1989.

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39

A comparison of rating water-source heat pumps using ARI standard 320 and ISO standard 13256-1. Gaithersburg, MD: U.S. Dept. of Commerce, Technology Administration, National Institute of Standards and Technology, 2001.

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40

Parker, Philip M. The 2007-2012 Outlook for Ground and Ground Water Source Heat Pumps in Greater China. ICON Group International, Inc., 2006.

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41

Parker, Philip M. The 2007-2012 Outlook for Ground and Ground Water Source Heat Pumps in the United States. ICON Group International, Inc., 2006.

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42

Source-area characteristics of large public surface-water supplies in the conterminous United States: An information resource for source-water assessment (U.S. Geological Survey open-file report). U.S. Geological Survey, 1999.

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43

Parker, Philip M. The 2007-2012 World Outlook for Water Source Heat Pump Unitary Air Conditioners Excluding Room Air Conditioners. ICON Group International, Inc., 2006.

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44

Parker, Philip M. The 2007-2012 Outlook for Water Source Heat Pump Unitary Air Conditioners Excluding Room Air Conditioners in Japan. ICON Group International, Inc., 2006.

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45

Parker, Philip M. The 2007-2012 Outlook for Water Source Heat Pump Unitary Air Conditioners Excluding Room Air Conditioners in India. ICON Group International, Inc., 2006.

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46

Economic evaluation of the closed loop water source heat pump system versus alternative HVAC systems with and without ... American Gas Association, 1987.

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47

Bridges, John C. Evolution of the Martian Crust. Oxford University Press, 2017. http://dx.doi.org/10.1093/acrefore/9780190647926.013.18.

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This is an advance summary of a forthcoming article in the Oxford Encyclopedia of Planetary Science. Please check back later for the full article.Mars, which has a tenth of the mass of Earth, has cooled as a single lithospheric plate. Current topography gravity maps and magnetic maps do not show signs of the plate tectonics processes that have shaped the Earth’s surface. Instead, Mars has been shaped by the effects of meteorite bombardment, igneous activity, and sedimentary—including aqueous—processes. Mars also contains enormous igneous centers—Tharsis and Elysium, with other shield volcanoes in the ancient highlands. In fact, the planet has been volcanically active for nearly all of its 4.5 Gyr history, and crater counts in the Northern Lowlands suggest that may have extended to within the last tens of millions of years. Our knowledge of the composition of the igneous rocks on Mars is informed by over 100 Martian meteorites and the results from landers and orbiters. These show dominantly tholeiitic basaltic compositions derived by melting of a relatively K, Fe-rich mantle compared to that of the Earth. However, recent meteorite and lander results reveal considerable diversity, including more silica-rich and alkaline igneous activity. These show the importance of a range of processes including crystal fractionation, partial melting, and possibly mantle metasomatism and crustal contamination of magmas. The figures and plots of compositional data from meteorites and landers show the range of compositions with comparisons to other planetary basalts (Earth, Moon, Venus). A notable feature of Martian igneous rocks is the apparent absence of amphibole. This is one of the clues that the Martian mantle had a very low water content when compared to that of Earth.The Martian crust, however, has undergone hydrothermal alteration, with impact as an important heat source. This is shown by SNC analyses of secondary minerals and Near Infra-Red analyses from orbit. The associated water may be endogenous.Our view of the Martian crust has changed since Viking landers touched down on the planet in 1976: from one almost entirely dominated by basaltic flows to one where much of the ancient highlands, particularly in ancient craters, is covered by km deep sedimentary deposits that record changing environmental conditions from ancient to recent Mars. The composition of these sediments—including, notably, the MSL Curiosity Rover results—reveal an ancient Mars where physical weathering of basaltic and fractionated igneous source material has dominated over extensive chemical weathering.
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48

A, Battaglin William, and Geological Survey (U.S.), eds. Estimating the susceptibility of surface water in Texas to nonpoint-source contamination by use of logistic regression modeling. [Reston, Va.]: U.S. Dept. of the Interior, U.S. Geological Survey, 2003.

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49

A, Battaglin William, and Geological Survey (U.S.), eds. Estimating the susceptibility of surface water in Texas to nonpoint-source contamination by use of logistic regression modeling. [Denver? Colo.]: U.S. Dept. of the Interior, U.S. Geological Survey, 2003.

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50

A, Battaglin William, and Geological Survey (U.S.), eds. Estimating the susceptibility of surface water in Texas to nonpoint-source contamination by use of logistic regression modeling. [Reston, Va.]: U.S. Dept. of the Interior, U.S. Geological Survey, 2003.

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