Abstract
Soil hydraulic conductivity (\(K\)) is an important soil property that exhibits relatively large uncertainty. The temporal variability of \(K\) is often ignored when calculating water movement in soil. Various factors such as tillage, rain, temperature, wetting/drying, soil surface crusting, solution concentration, and biological activity can influence field \(K\). We investigated soil \(K\) in a central Iowa field as a function of time and tillage by using tension infiltrometer measurements with pressure head tension settings of 0 cm and − 3 cm. No clear relationship was found between bulk density (\(\rho_{\text{b}}\)) and \(K\). Path analysis was conducted to assess the contribution ratios and causal relationships between factors affecting \(K\). The \(K\) values were influenced by physical impacts such as tillage, precipitation, and surface crusting with contributions of 24%, − 32%, and 49%, respectively, and with error of 60%. Soil surface crusting had a particularly large impact on saturated \(K\). The maximum volume fraction influenced \(K\). Earthworm activity that impacted the soil pore structure was also noticed in the field. Owing to this biological mechanism, no relationship was observed between \(\rho_{\text{b}}\) and \(K\). It is important to recognize the multiple combined effects of soil physical processes and biological activities when documenting \(K\) in field soils.
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Acknowledgements
Thanks to Dr. Sally D. Logsdon for her kind advice and help in the early stages of this work, to Dr. Dilia Kool, Dr. Zhuangji Wang, Mr. Bing Tong and Mr. Ohene Akuoko for help in the field measurements, and to Dr. Takeshi Tokida, National Agriculture and Food Research Organization, for covariance analysis guidance. This work was supported in part by the USA National Science Foundation under grant 1623806, the USA Army Research Office under grant W911NF-16-1-0287, USDA-NIFA, the Hatch Act, and State of Iowa funds, and Ibaraki University. We also would like to thank Editage (www.editage.com) for English language editing.
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Nishiwaki, J., Horton, R. Temporal changes in soil hydraulic conductivity in saturated and unsaturated fields. Paddy Water Environ 18, 677–686 (2020). https://doi.org/10.1007/s10333-020-00810-x
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DOI: https://doi.org/10.1007/s10333-020-00810-x