Groundwater

From 2007 to 2021, the U.S. Geological Survey (USGS) collaborated with the Nevada Bureau of Mines and Geology on evaluating the forms of arsenic in Nevada groundwater resources. A total of 190 groundwater samples were collected from wells and springs throughout Nevada. Concentrations of arsenic ranged from <1.6 to 2,408 micrograms per liter (µg/L); in most cases, arsenate was the dominant species...

High concentrations of phosphorus (P) and nitrogen (N) are responsible for excessive, or nuisance algal blooms in many ecosystems world-wide, and climate change is predicted to exacerbate the problem1,2. Excessive nutrients supplied to the nearshore zone of Lake Tahoe may have significant consequences to ecological communities, water clarity, and water quality. The nearshore zone represents the...

The multidisciplinary research team is made up of scientists from research institutes, universities, National laboratories, and the USGS. The USGS co-leaders for the team are Brian J. Andraski (ADRS Coordinator, Nevada Water Science Center) and David A. Stonestrom (National Research Program, California).

The Amargosa Desert Research Site (ADRS), in the northern Mojave Desert, is about 20 km east of Death Valley National Park. Recognizing the paucity of information on unsaturated-zone hydrology in arid regions, the USGS, in 1983, established the ADRS through agreements with the Bureau of Land Management (BLM) and the State of Nevada. The ADRS serves as a field laboratory for the study of arid-land...

In 1976, the U.S. Geological Survey (USGS) began studies of unsaturated zone hydrology at a site in the Amargosa Desert near Beatty, Nevada, as part of the USGS Low-Level Radioactive Waste Program. The site is near disposal trenches for civilian waste. Over the years, USGS investigations at the Amargosa Desert Research Site (ADRS) have provided long-term "benchmark" information about the hydraulic...

The Nevada Water Science Center (NVWSC) is increasing the spatial understanding of the distribution of arsenic and important geochemical information in groundwater resources near select water-supply wells in southern Carson Valley by collecting groundwater samples to complement the existing dataset (2006 – 2015).

The Virginia City Highlands and Highland Ranches (VC Highlands) are a rural residential housing area established along the ridge of the Virginia Range in Storey County, Nevada. Approximately 1,400 residents exclusively rely on domestic wells for water supply and domestic well depths range from 75 to 1,175 ft below land surface. NVWSC monitors water levels annually in two domestic wells in the VC...

The USGS National Water-Quality Assessment Project (NAWQA) is now part of the USGS National Water-Quality Program (NWQP). NAWQA provides nationally consistent data and information on the quality of the Nation’s water. Studies provide information on current water-quality conditions, a baseline for trend evaluation, and an understanding of what factors affect water quality. Groundwater studies for...

The U.S. Geological Survey (USGS) office in Henderson, Nevada, provides hydrologic, geologic, and other scientific and technical expertise to the U.S. Department of Energy (DOE) to address environmental and scientific issues at the Nevada National Security Site (NNSS) and vicinity.

Many aquifer tests have been conducted by the U.S. Geological Survey to estimate hydraulic properties of aquifers in Nevada and adjacent states. Transmissivity is the principal hydraulic property that has been estimated from the aquifer tests in Nevada because these values directly affect estimates of ground-water flow.

Evapotranspiration (ET) is the process that transfers water from land surface to the atmosphere as evaporation (or sublimation when below freezing) from open water, soil, and plant canopies and as transpiration by plants. ET is measured by scientists for many different reasons. Hydrologists from the Nevada Water Scientist Center (NVWSC) typically measure ET to help quantify water budgets...

The Colorado River is one of the longest rivers in the Western United States. It begins in the Rocky Mountains of Colorado and flows southwestward until it reaches Mexico where it becomes a small stream or dry riverbed. The Colorado River forms the border between southeastern Nevada and northwestern Arizona. In Nevada, Hoover Dam and Davis Dam control the flow of the river and create two...