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Roswell Artesian Basin

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The Roswell Artesian Basin is located in the lower Pecos Valley of southeastern New Mexico, on the northern fringe of the Chihuahua Desert. Summers are long and hot and precipitation is sparse, averaging less than 15 inches/year. However, the Roswell Basin is also one of the most intensively farmed areas in the state, the principal crops being alfalfa, cotton, sorghum, chiles and pecans. The Basin derives virtually all of its irrigation water from groundwater stored in a shallow alluvial aquifer and an artesian aquifer formed principally in the San Andres limestone. The Roswell Artesian Basin has been described as a world-class example of a rechargeable artesian aquifer system.

Hydrologic investigations of the Roswell Basin began in 1906 with Fisher’s report of early hydraulic head conditions. In 1933 Fiedler and Nye conducted a much more comprehensive study of the geology and water resources of the lower Pecos region. Their report identified the principal features of the artesian and shallow aquifers and provided a foundation for subsequent work, much of it conducted by scientists with the U.S. Geological Survey and the New Mexico Office of the State Engineer.

In 1957 Mahdi Hantush, one of the founders of the hydrology department at New Mexico Tech, published an analytical study of the Basin and defined aquifer coefficients based on pumping tests. Hood and colleagues (1960; 1963) documented the occurrence of saline groundwater in the artesian aquifer. Motts and Cushman (1964) investigated the possibility of artificial recharge to the aquifer through surface karst features developed in the San Andres limestone. In 1968 Havenor published a New Mexico Bureau of Mines Circular describing lithology and structural relationships within the artesian aquifer, which includes a detailed description of a complete core taken from the San Andres Formation. In 1971 Vince Kelley published a Bureau of Mines Memoir and set of maps on regional geology of the Pecos Country in southeastern New Mexico. Although Kelley’s work was not specifically hydrological, much of the report focuses on lithostratigraphy of the San Andres limestone, and thus provides valuable regional context for hydrologic studies in the Artesian Basin.

In the late 1970s and early 80s, students from New Mexico Tech, under the supervision of Dr. Gerardo Gross, conducted a series of investigations on groundwater flow rates and subsurface recharge to the artesian aquifer using tritium and stable isotope measurements. Most of their work was published in technical reports of the New Mexico Water Resources Research Institute. In 1983 G. E. Welder, a hydrologist with the U.S. Geological Survey, published a comprehensive report and series of maps showing water level variations in the Roswell Artesian Basin. Welder’s report was extended by Land (2007; 2008) based on new water level measurements. Additional studies by Land focus on groundwater residence time and the karstic nature of the artesian aquifer system.

A short list of the most-frequently cited publications that focus on hydrology and hydrogeology of the Roswell Artesian Basin and its recharge areas on the Pecos Slope and in the Sacramento Mountains is shown below.

Open-file Report 503:

Available for free download.

Seasonal and long term variations in hydraulic head in a karstic aquifer: Roswell Artesian Basin, New Mexico, 2007, Lewis Land and Brad T. Newton

Open-file Report 521:

Available for free download.

Multi-tracer investigation of groundwater residence time in a karstic aquifer: Bitter Lake National Wildlife Refuge, New Mexico, 2010, Lewis Land and G. F. Huff

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Selected References

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