TY - JOUR
T1 - A geometric equation for representing morphological field information in horizons with compound structure
AU - Hirmas, Daniel
AU - Giménez, Daniel
N1 - Funding Information:
We thank Aoesta Mohammed for compiling the structure data that was used to initially test the proposed equation. Daniel Giménez acknowledges support from the National Institute of Food and Agriculture, U.S. Department of Agriculture, Hatch project 1008886 through the New Jersey Agricultural Experiment Station, Hatch project NJ07235. The comments from two anonymous reviewers helped strengthen the manuscript.
Publisher Copyright:
© Soil Science Society of America, 5585 Guilford Rd., Madison WI 53711 USA. All Rights reserved
PY - 2017/7/1
Y1 - 2017/7/1
N2 - Recent advances in the quantification of ped geometry have revealed a need to integrate the values obtained from individual peds within horizons that contain multiple ped sizes, grades, and/or types. Here we propose a general equation to represent with a single value the structural character of a horizon that may contain single, multiple, and/or compound structure. The equation is based on the calculation of a weighting parameter from estimates of the vertical cross-sectional area of each unique structure class present in a horizon. The equation can be used to integrate quantifiable aspects of either structure size, grade, or shape. We demonstrate the usefulness of this equation in two soils—the Alloway series (Aquic Paleudults) and Holdredge series (Typic Argiustolls)—that exhibit multiple or compound structure in each horizon. This work may extend the applicability of structural information from previously described soils, enhance existing profile development indices, and aid the formulations of mechanistic soil hydrological models that account for the depth distributions of soil structural properties.
AB - Recent advances in the quantification of ped geometry have revealed a need to integrate the values obtained from individual peds within horizons that contain multiple ped sizes, grades, and/or types. Here we propose a general equation to represent with a single value the structural character of a horizon that may contain single, multiple, and/or compound structure. The equation is based on the calculation of a weighting parameter from estimates of the vertical cross-sectional area of each unique structure class present in a horizon. The equation can be used to integrate quantifiable aspects of either structure size, grade, or shape. We demonstrate the usefulness of this equation in two soils—the Alloway series (Aquic Paleudults) and Holdredge series (Typic Argiustolls)—that exhibit multiple or compound structure in each horizon. This work may extend the applicability of structural information from previously described soils, enhance existing profile development indices, and aid the formulations of mechanistic soil hydrological models that account for the depth distributions of soil structural properties.
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U2 - 10.2136/sssaj2016.12.0396n
DO - 10.2136/sssaj2016.12.0396n
M3 - Article
AN - SCOPUS:85028721520
VL - 81
SP - 863
EP - 867
JO - Soil Science Society of America Journal
JF - Soil Science Society of America Journal
SN - 0361-5995
IS - 4
ER -