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Post-tillage evolution of structural pore space and saturated and near-saturated hydraulic conductivity in a clay loam soil
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文摘

Volume of pores >0.5 mm in size decreased within one month after harrowing.

This reduced field-saturated hydraulic conductivity, but not laboratory measured Ks.

Sample-scale connectivity of pores large than 0.5 mm in diameter was always limited.

Ks was correlated with imaged porosity <0.5 mm in size and global pore connectivity.

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