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Saturated Hydraulic Conductivity Variation in Cultivated and Virgin Soils

机译:耕地和原生土壤的饱和导水率变化

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Variation of saturated hydraulic conductivity (Ks) values of soils under diverse management practices may be needed to determine the required sample number, sample size, and chose suitable sample scheme for characterize the Ks values used in water flow and solute transport modelling studies. The purpose of this study was to examine the variability in Ks and try to understand some part of the determinism of this variability in virgin and adjacent cultivated field using 36 undisturbed soil samples from each location with 0.5-m grid space. Ks was measured with 100 cm3 undisturbed soil cores in laboratory using falling or constant head methods. The results showed that variability of ln (Ks) values (variance = 10.3) at the cultivated site was 2.5 times greater than that (variance = 2.5) at the virgin site. Furthermore, significant Ks differences exist between cultivated sample locations and within the rows of each cultivated location. Greater variations occurred in two cultivated locations may be attributed to compaction by traffic and soil tillage resulting in heterogeneous bulk density over the study area.
机译:为了确定所需的样本数量,样本量,并选择合适的样本方案来表征水流和溶质运移模型研究中所使用的Ks值,可能需要在各种管理实践下改变土壤的饱和导水率(Ks)值。这项研究的目的是检查Ks的变异性,并尝试使用0.5 m网格空间的每个位置的36个未扰动土壤样本来了解原始和邻近耕地中这种变异性的确定性。在实验室中使用落头法或恒定水头法在100 cm3的原状土壤芯中测量Ks。结果表明,栽培部位的ln(Ks)值变异性(方差= 10.3)比原始部位的ln(Ks)值变异性(方差= 2.5)大2.5倍。此外,在栽培样品位置之间以及每个栽培位置的行内存在明显的Ks差异。在两个耕种地点发生的较大变化可能归因于交通和土壤耕作造成的压实,从而导致研究区域的堆积密度不均匀。

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