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Effects of drip irrigation on migration and distribution of heavy metals in soil profile

机译:滴灌对土壤剖面重金属迁移和分布的影响

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Drip irrigation systems have been widely applied in semiarid and arid regions of China. However, little is known about the migration of heavy metals in cultivated soil under drip irrigation. Therefore, the concentrations of Cd, Cr, Cu, Ni, Pb, and Zn in soil were determined. The mean contents of Cd, Cr, Cu, Pb, Zn, and Ni in surface soil subjected to irrigation with low and high amounts of water (W1 and W2) were 0.11, 117.50, 37.51, 13.53, 78.10, and 38.41 mg/kg and 0.20, 94.45, 29.71, 22.48, 63.00, and 36.62 mg/kg, respectively. Metal concentrations in deep soil varied slightly between W1 and W2. Among different distances from the dropper, the metal levels in surface soil varied widely, while they varied slightly in deep soil. The I (geo) (geo-accumulation index) values indicated that the soil was usually contaminated by Cr, Cu, and Cd. Under W1, Cd and Cu usually accumulated in surface soil near the dropper, while the other metals leached into subsurface soil. Moreover, the metals generally accumulated in soil away from the dropper. However, significant leaching of metals to the subsurface and deep soil was observed near the dropper under W2. Away from the dropper, Cd, Cr, Cu, Ni, and Pb usually accumulated in surface and deep soil. This suggested that heavy metals generally migrated to the soil away from the dropper when subjected to lower amounts of irrigation, while metals usually moved to surface soil and deep soil under high irrigation amounts. These findings indicate that drip irrigation greatly affected the distribution and migration of heavy metals in soil, with irrigation with lower amounts of irrigation water significantly affecting the horizontal migration of heavy metals and higher amounts influencing the vertical movement of heavy metals.
机译:滴灌系统已在中国半干旱和干旱地区得到广泛应用。然而,对于滴灌条件下耕种土壤中重金属的迁移知之甚少。因此,测定了土壤中Cd,Cr,Cu,Ni,Pb和Zn的浓度。分别以低量和高量水(W1和W2)灌溉的表层土壤中Cd,Cr,Cu,Pb,Zn和Ni的平均含量为0.11、117.50、37.51、13.53、78.10和38.41 mg / kg和0.20、94.45、29.71、22.48、63.00和36.62 mg / kg。在W1和W2之间,深层土壤中的金属浓度略有不同。在距滴管不同距离的地方,表层土壤中的金属含量变化很大,而深层土壤中的金属含量变化很小。 I(geo)(地理积累指数)值表明土壤通常被Cr,Cu和Cd污染。在W1下,Cd和Cu通常聚集在滴管附近的表层土壤中,而其他金属则渗入地下土壤中。而且,金属通常在远离滴管的地方积聚在土壤中。然而,在W2下滴管附近观察到金属大量浸入地下和深层土壤。除滴管外,Cd,Cr,Cu,Ni和Pb通常累积在表层和深层土壤中。这表明,当灌溉量较低时,重金属通常会从滴管移到土壤中,而灌溉量较大时,金属通常会移至表层土壤和深层土壤。这些发现表明,滴灌对土壤中重金属的分布和迁移有很大影响,而灌溉水量少的灌溉水会显着影响重金属的水平迁移,而大量灌溉会影响重金属的垂直运动。

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