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Temporal-spatial distribution and variability of cadmium contamination in soils in Shenyang Zhangshi irrigation area, China

机译:沉阳张氏灌区土壤镉污染的时空分布及其变异性

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Heavy metal contamination in soils has been of wide concern in China in the last several decades. The heavy metal contamination was caused by sewage irrigation, mining and inappropriate utilization of various agrochemicals and pesticides and so on. The Shenyang Zhangshi irrigation area (SZIA) in China is a representative area of heavy metal contamination of soils resulting from sewage irrigation for about 30 years duration. This study investigated the spatial distribution and temporal variation of soil cadmium contamination in the SZIA. The soil samples were collected from the SZIA in 1990 and 2004; Cd of soils was analyzed and then the spatial distribution and temporal variation of Cd in soils was modelled using kriging methods. The kriging map showed that long-term sewage irrigation had caused serious Cd contamination in topsoil and subsoil. In 2004, the Cd mean concentrations were 1.698 and 0.741 mg/kg, and the maxima 10.150 and 7.567 mg/kg in topsoils (0-20 cm) and subsoils (20-40 cm) respectively. These values are markedly more than the Cd levels in the second grade soil standard in China. In 1990, the Cd means were 1.023 and 0.331 mg/kg, and the maxima 9.400 and 3.156 mg/kg, in topsoils and subsoils respectively. The soil area in 1990 with Cd more than 1.5 mg/kg was 2701 and 206.4 hm~2 in topsoils and subsoils respectively; and in 2004, it was 7592 and 1583 hm~2, respectively. Compared with that in 1990, the mean and maximum concentration of Cd, as well as the soil area with Cd more than 1.5 mg/kg had all increased in 2004, both in topsoils and subsoils.
机译:在过去的几十年中,土壤中的重金属污染一直是中国广泛关注的问题。重金属污染是由污水灌溉,采矿以及各种农药和农药的不当使用等引起的。中国的沉阳张石灌区(SZIA)是污水灌溉造成的土壤重金属污染的典型地区,持续了约30年。这项研究调查了SZIA中土壤镉污染的空间分布和时间变化。土壤样品分别于1990年和2004年从SZIA采集。分析土壤中的镉,然后使用克里格法对土壤中镉的空间分布和时间变化进行建模。克里金图显示,长期的污水灌溉已在表土和底土中引起严重的Cd污染。 2004年,镉的平均浓度分别为1.698和0.741 mg / kg,表层土壤(0-20厘米)和地下土壤(20-40厘米)的最大值分别为10.150和7.567毫克/公斤。这些值明显高于中国二级土壤标准中的Cd水平。 1990年,表层土壤和下层土壤的Cd平均值分别为1.023和0.331 mg / kg,最大值为9.400和3.156 mg / kg。 1990年Cd大于1.5 mg / kg的土壤表层土壤和下层土壤分别为2701和206.4 hm〜2。 2004年分别为7592和1583 hm〜2。与1990年相比,2004年Cd的平均浓度和最大浓度以及Cd大于1.5 mg / kg的土壤面积在表土和地下土壤中均增加。

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