結論

不像人工創造的穩定的驅蟲表面或多孔 介質，拒水土壤表現出潤濕動力學，由此 最初疏水的土壤隨著時間的推移變得親水 與水接觸時。 初始潤濕動力學 排斥土壤通常歸因于 固液界面能 (γSL)，或液汽界面能 (γLV) 的降低，或兩者兼而有之。 γLV 的減少 建議是由于土壤表面溶解 活性有機化合物進入與水接觸的水中 土壤。 在這項研究中，我們測試了土傳表面的影響 潤濕動力學的活性物質，并發現，與廣為接受的范式相反，土壤釋放表面 活性化合物不會加速潤濕過程。 因此很明顯，固體界面能的變化 表面（γSL 或 γSV），而不是液汽 表面 (γLV) 必須在驅動不穩定排斥性土壤的潤濕動力學方面起主導作用。

致謝

本研究由以色列農業部資助 和農村發展，資助號 821-0088-04。

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表面活性劑是否對斥水性土壤的潤濕性有影響？——概括、介紹

表面活性劑是否對斥水性土壤的潤濕性有影響？——材料和方法

表面活性劑是否對斥水性土壤的潤濕性有影響？——結果和討論

表面活性劑是否對斥水性土壤的潤濕性有影響？——結論、致謝！