Premium
POLARIS Soil Properties: 30‐m Probabilistic Maps of Soil Properties Over the Contiguous United States
Author(s) -
Chaney Nathaniel W.,
Minasny Budiman,
Herman Jonathan D.,
Nauman Travis W.,
Brungard Colby W.,
Morgan Cristine L. S.,
McBratney Alexander B.,
Wood Eric F.,
Yimam Yohannes
Publication year - 2019
Publication title -
water resources research
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 1.863
H-Index - 217
eISSN - 1944-7973
pISSN - 0043-1397
DOI - 10.1029/2018wr022797
Subject(s) - soil series , soil map , digital soil mapping , soil survey , soil science , soil water , environmental science , pedotransfer function , soil texture , hydrology (agriculture) , soil horizon , hydraulic conductivity , geology , soil classification , geotechnical engineering
Soils play a critical role in the cycling of water, energy, and carbon in the Earth system. Until recently, due primarily to a lack of soil property maps of a sufficiently high‐quality and spatial detail, a minor emphasis has been placed on providing high‐resolution measured soil parameter estimates for land surface models and hydrologic models. This study introduces Probabilistic Remapping of SSURGO (POLARIS) soil properties—a database of 30‐m probabilistic soil property maps over the contiguous United States (CONUS). The mapped variables over CONUS include soil texture, organic matter, pH, saturated hydraulic conductivity, Brooks‐Corey and Van Genuchten water retention curve parameters, bulk density, and saturated water content. POLARIS soil properties was assembled by (1) depth harmonizing and aggregating the pedons in the National Cooperative Soil Survey Soil Characterization Database and the components in Soil Survey Geographic Database into a database of 21,481 different soil series, each soil series having its own vertical profiles of different soil properties, (2) pruning the original POLARIS soil series maps using conventional soil maps to improve soil series prediction accuracy, and (3) merging the assembled soil series databases with the pruned POLARIS soil series maps to construct the soil property maps over CONUS. POLARIS soil properties includes 100‐bin histograms for each layer and variable per grid cell and a series of summary statistics at 30‐, 300‐, and 3,000‐m spatial resolution. Evaluation of POLARIS soil properties using in situ measurements shows an average R 2 of 0.41, normalized root‐mean‐square error of 12%, and a normalized mean absolute error of 8.8%.