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Broad-scale assessment of biophysical features in Colorado: Soil salinity using electrical conductance

Published by U.S. Geological Survey | Department of the Interior | Metadata Last Checked: January 27, 2026 | Last Modified: 2020-08-20T00:00:00Z
This dataset “Broad-scale assessment of biophysical features in Colorado: Soil salinity using electrical conductance” presents information extracted from the Natural Resources Conservation Service (NRCS) gridded surface soils geographic database (gSSURGO). Fields retained and presented here include map unit (MU) codes and component (COMP) codes that may be used to reference records in the original, NRCS, data. Soil salinity is typically measured and evaluated based on electrical conductance (EC), and values presented here include the representative value for the map unit component (ECR) and the highest estimated value (ECH). Soils with high salinity can affect the composition of vegetation and can limit production of plants through effects on leaf water potential and water use efficiency. Elevated salinity is often created by geologic and soil moisture relations that promote movement of salts. Salt levels can increase as a result of cropping, irrigation and land management. Salinity is typically measured using electrical conductance in wet soils; soils with electrical conductance less than 2 millimhos (mmhos)/centimeter (cm) are non-saline, 2 to less than 4 mmhos/cm are very slightly saline, 4 to less than 8 mmhos/cm are slightly saline, 8 to less than16 mmhos/cm are moderately saline, and greater than or equal to 16 mmhos/cm are strongly saline. Millimhos/centimeter is the traditional unit for soil EC measurement; it is equivalent to the accepted scientific unit, decisiemens/meter (dS/m). Review of information regarding EC and salinity from the source (NRCS) is suggested: https://www.nrcs.usda.gov/wps/portal/nrcs/detail/national/home/?cid=nrcs144p2_065177 and (or) https://www.nrcs.usda.gov/Internet/FSE_DOCUMENTS/nrcs142p2_053280.pdf.

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