Relationship Between Solute Diffusion Coefficient and Electrical Conductivity Under Extremely Low Soil Water Conditions
Relationship Between Solute Diffusion Coefficient and Electrical Conductivity Under Extremely Low Soil Water Conditions
复制标题
极低土壤水分条件下溶质扩散系数与电导率的关系
DOI:
10.1007/s42729-022-00792-1
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发表时间:
2022
影响因子:
3.9
通讯作者:
Sho Shiozawa
中科院分区:
文献类型:
--
作者:
Katori Miyasaka;Sho Shiozawa
The relative diffusion coefficient (Dr) of solutes in soils is directly proportional to the “nth” power of the volumetric soil water content (θ), wherenis an empirical parameter, which normally ranges between 1 and 2. The existence of a breakpoint (θbr) in the relationship betweenθandDrhas been demonstrated at low-θ, in which the value ofnbecomes approximately 4 whenθ<θbr. The change inncan be attributed to various mechanisms, including drastic changes in the geometrical distribution of pore liquid water caused by dehydration. However, as directDrmeasurements require considerable time to render sufficient data at low-θ, few studies have measuredDratθ<θbr, and the relationship betweenDrandθatθ<θbrremains unclear. In this study, we investigated if the indirectDrmeasurement method can be applied in the low-θregion ofθ<θbr. An indirect method for measuringDrwas employed to determine the soil electrical conductivity (ECs). Using dune sands in which the presence ofθbrwas confirmed,Drfrom high- to low-θwas calculated based on ECsmeasurements and compared with directly measuredDr. The relationships betweenθandDrcalculated based on ECsand using the transient state method were almost the same.Drcould be calculated from ECseven atθ<θbr. The results confirmed that the indirect Dr measurement method can be applied for the low-θregion ofθ<θbr.