Fact Sheet 2012–3098
The Coachella Study Area
The Coachella study area is approximately 820 square miles (2,124 square kilometers) and includes the Coachella Valley groundwater basin (California Department of Water Resources, 2003). Coachella Valley has an arid climate, with average annual rainfall of about 6 inches (15 centimeters). The runoff from the surrounding mountains drains to rivers that flow east and south out of the study area to the Salton Sea. Land use in the study area is approximately 67 percent (%) natural, 21% agricultural, and 12% urban. The primary natural land cover is shrubland. The largest urban areas are the cities of Indio and Palm Springs (2010 populations of 76,000 and 44,000, respectively).
Groundwater in this basin is used for public and domestic water supply and for irrigation. The main water-bearing units are gravel, sand, silt, and clay derived from surrounding mountains. The primary aquifers in Coachella Valley are defined as those parts of the aquifers corresponding to the perforated intervals of wells listed in the California Department of Public Health database. Public-supply wells in Coachella Valley are completed to depths between 490 and 900 feet (149 to 274 meters), consist of solid casing from the land surface to a depth of 260 to 510 feet (79 to 155 meters), and are screened or perforated below the solid casing. Recharge to the groundwater system is primarily runoff from the surrounding mountains, and by direct infiltration of irrigation. The primary sources of discharge are pumping wells, evapotranspiration, and underflow to the Salton Sea and Imperial Valley areas.
Overview of Water Quality
GAMA’s Priority Basin Project evaluates the quality of untreated groundwater. However, for context, benchmarks established for drinking-water quality are used for comparison. Benchmarks and definitions of high, moderate, and low concentrations are discussed in the inset box on page 3. The USGS sampled 19 wells for this assessment; data from the California Department of Public Health database were used to supplement USGS data.
Many inorganic constituents occur naturally in groundwater. The concentrations of the inorganic constituents can be affected by natural processes as well as by human activities. In the Coachella study area, one or more inorganic constituents were present at high concentrations in 42% of the primary aquifers and at moderate concentrations in 26%.
Organic constituents are found in products used in the home, business, industry, and agriculture. Organic constituents can enter the groundwater system through normal usage, spills, or improper disposal. In the Coachella study area, organic constituents were present at moderate concentrations in 1% of the primary aquifers.
RESULTS: Groundwater Quality in the Coachella Study Area
Inorganic Constituents with Human-Health Benchmarks
Trace elements are naturally present in the minerals in rocks and soil, and in the water that comes into contact with those materials. In the Coachella study area, trace elements with human-health benchmarks were present at high concentrations in 37% of the primary aquifers. Trace elements were present at moderate concentrations in 21% of the primary aquifers. Of the 17 trace elements with human-health benchmarks analyzed in this study, 5 were detected at high concentrations: arsenic, boron, fluoride, molybdenum, and strontium. Vanadium was present at moderate concentrations.
Radioactivity is the release of energy or energetic particles during structural changes in the nucleus of an atom. Most of the radioactivity in groundwater comes from decay of naturally occurring isotopes of uranium and thorium that are present in minerals in the aquifer. In the Coachella study area, radioactive constituents were detected at concentrations above benchmarks in 4% of the primary aquifers, and at moderate concentrations in 10%. Six radioactive constituents were analyzed; of these, uranium and gross alpha radioactivity were detected at concentrations above benchmarks.
Nutrients, such as nitrate and nitrite, are naturally present at low concentrations in groundwater. High and moderate concentrations generally occur as a result of human activities, such as fertilizer application, livestock waste, or septic-system seepage. Of the three nutrients with health-based benchmarks analyzed, one, nitrate, was detected at concentrations above benchmarks in the Coachella primary aquifers.
Inorganic Constituents with Non-Health Benchmarks
(Not included in water-quality overview charts shown on the front page)
Other inorganic constituents, such as total dissolved solids and manganese, affect the aesthetic properties of water, such as taste, color, or odor. In the Coachella study area, these constituents were present at high concentrations in 16% of the primary aquifers, and at moderate concentrations in 21%. Of the seven constituents with non-health-based benchmarks analyzed, four were detected at concentrations above benchmarks: chloride, manganese, total dissolved solids, and sulfate.
Special Interest: Perchlorate
Perchlorate is an inorganic constituent that has been regulated in California drinking water since 2007. It is an ingredient in rocket fuel, fireworks, safety flares, may be present in some fertilizers, and also occurs naturally at low concentrations in groundwater. In the Coachella study area, perchlorate was found at high concentrations in 10% and at moderate concentrations in 16% of the primary aquifers.
Organic Constituents with Human-Health Benchmarks
The Priority Basin Project uses laboratory methods that can detect the presence of volatile organic compounds (VOCs) and pesticides at very low concentrations, far below human-health benchmarks. VOCs and pesticides detected at these very low concentrations can be used to help trace water from the land surface into the aquifer system.
Volatile Organic Compounds
VOCs are present in many household, commercial, industrial, and agricultural products, and are characterized by their tendency to volatilize into the air. Of 56 VOCs with health-based benchmarks analyzed in the Coachella study area, none were detected above benchmarks. The VOCs trichloromethane and tetrachloroethene were detected at moderate concentrations in 1% of the Coachella primary aquifers.
Pesticides are used on lawns, in gardens, around buildings, along roads, and in agriculture to help control unwanted vegetation (weeds), insects, fungi, and other pests. In the Coachella study area, pesticides were not detected or only detected at low concentrations. Of the 20 pesticides with health-based benchmarks that were analyzed in the Coachella primary aquifers, none were detected at high or moderate concentrations in the primary aquifers.
BENCHMARKS FOR EVALUATING GROUNDWATER QUALITY
GAMA’s Priority Basin Project uses benchmarks established for drinking water to provide context for evaluating the quality of untreated groundwater. After withdrawal, groundwater may be disinfected, filtered, mixed, or exposed to the atmosphere before being delivered to consumers. Federal and California regulatory benchmarks for protecting human health (Maximum Contaminant Level, MCL) are used when available. Otherwise, nonregulatory benchmarks for protecting human health (Notification Level, NL, and Lifetime Health Advisory, HAL) and nonregulatory benchmarks for protecting aesthetic properties such as taste and odor (Secondary Maximum Contaminant Level, SMCL) are used.
High, moderate, and low concentrations are defined relative to benchmarks
Concentrations are considered high if they are greater than a benchmark. For inorganic constituents, concentrations are moderate if they are greater than one-half of a benchmark. For organic and special-interest constituents, concentrations are considered moderate if they are greater than one-tenth of a benchmark; this lower threshold was used because organic constituents are generally less prevalent and have smaller concentrations relative to benchmarks than inorganic constituents. Low concentrations include non-detections and values less than moderate concentrations. Methods for evaluating water quality are discussed by Milby Dawson and Belitz (2012).
Trace Element Concentrations Throughout the California Desert Region
Trace elements were present at high concentrations in all of the Desert Region primary aquifers. In the Coachella study area, they were high in 37% of the primary aquifers, on an areal basis; the range of high trace element percentages in the Desert Region primary aquifers was 15 to 54% (Milby Dawson and Belitz, 2012). The trace elements with the highest percentages in Coachella were arsenic (high in 21% of the primary aquifers) and fluoride (21%). Arsenic was found at high concentrations in all of the primary aquifers in the Desert region. Fluoride was found at high concentrations in five of the six Desert Region study areas and in the highest proportion in Coachella.
Priority Basin Assessments
GAMA’s Priority Basin Project (PBP) assesses water quality in that part of the aquifer system used for drinking water, primarily public supply. Water quality in shallower and deeper parts may differ from water quality in the primary aquifers. GAMA’s Domestic Well Project assesses water quality in the shallower parts of the aquifer system. Ongoing assessments are being conducted in more than 120 basins throughout California.
The PBP assessments are based on a comparison of constituent concentrations in untreated groundwater with benchmarks established for the protection of human health and for aesthetic concerns. The PBP does not evaluate the quality of drinking water delivered to consumers.
The PBP uses two approaches for assessing groundwater quality. The first approach uses a network of wells to provide a statistically based assessment of the status of groundwater quality. The second approach uses additional wells to help assess the factors that affect water quality. Both approaches use data routinely collected for regulatory compliance, as well as data collected by the PBP. The PBP includes chemical analyses not generally available as part of regulatory compliance monitoring, including measurements at concentrations much lower than human-health benchmarks, and measurement of constituents that can be used to trace the sources and movement of groundwater.
California Department of Water Resources, 2003, California’s groundwater: California Department of Water Resources Bulletin 118, 246 p., available at http://www.water.ca.gov/groundwater/bulletin118/update2003.cfm
Goldrath, D.A., Wright, M.T., and Belitz, K., 2009, Ground-water quality data in the Coachella Valley study unit, 2007—Results from the California GAMA Program: U.S. Geological Survey Data Series 373, 70 p., available at http://pubs.usgs.gov/ds/373
Milby Dawson, B.J., and Belitz, K., 2012, Status of groundwater quality in the California Desert Region, 2006–2008—California GAMA Program Priority Basin Project: U.S. Geological Survey Scientific Investigations Report 2012-5040, 100 p.
First posted January 9, 2013
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Dawson, B.J.M., and Belitz, Kenneth, 2012, Groundwater quality in Coachella Valley, California: U.S. Geological Survey Fact Sheet 2012–3098, 4 p.