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通过田间灌溉试验获得的分室模型表明，随着灌溉水中ＮａＣｌ含量的增加，土壤水溶性Ｃｌ－、Ｎａ＋呈直线增加。Ｃｌ－增加的斜率明显大于Ｎａ＋。Ｃａ２＋和Ｍｇ２＋亦增加，矿化灌溉水中９６～９９％的Ｎａ＋，９７～９９％的Ｃｌ－存留在土壤中，进入作物体中则很少。在小麦中，Ｎａ＋、Ｃｌ－主要分布于茎、鞘中，占吸入总量的６５％左右，进入根和籽粒的Ｎａ＋占８～１０％，Ｃｌ－仅占３～６％。在甜菜中，Ｎａ＋、Ｃｌ－主要集中于叶和枯叶，占吸入总量的９０％以上，根中Ｎａ＋和Ｃｌ－均小于１０％。
The compartment model obtained from field irrigation experiments showed that the water-soluble Cl- and Na + increased linearly with the increase of NaCl in irrigation water. The slope of Cl-increase is significantly greater than Na +. Ca2 + and Mg2 + also increased. 96-99% of Na + and 97-99% of Cl- in mineralized irrigation water were retained in the soil, and few were found in the crop. In wheat, Na + and Cl- are mainly distributed in stems and sheaths, accounting for about 65% of the total amount of inhaled rice, 8-10% of Na + entering roots and grains, and 3-6% of Cl-. In sugar beet, Na + and Cl- mainly concentrate on leaves and dead leaves, accounting for more than 90% of the total amount of inhalation. Na + and Cl- in roots are less than 10%.