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首页> 外文期刊>Journal of soil science and plant nutrition >Nitrification and nitrogen mineralization in agricultural soils contaminated by copper mining activities in Central Chile
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Nitrification and nitrogen mineralization in agricultural soils contaminated by copper mining activities in Central Chile

机译:智利中部铜矿开采活动污染的农业土壤中的硝化作用和氮矿化作用

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Microbiological bioassays of nitrification and nitrogen mineralization have been used for evaluation of soil quality on metal-contaminated soils. We evaluated the effectiveness of nitrification and nitrogen mineralization bioassays as quality indicators of soil degradation caused by metal contamination. We performed standard tests based on protocols of ISO 14238 (2012) and ISO 15685 (2012) on 90 soil samples collected from agricultural areas in central Chile that were historically contaminated by mining activities. Potential nitrification rate (PNR) was best explained by pH and organic matter content (OM) (R2=0.32), while nitrogen mineralization (Nmin) was best explained by OM and clay content (R2=0.44). Following normalization of the bioassays responses with respect to OM yielded significant correlations between PNR and pH and total Cu content (R2=0.22), and between Nmin and clay and total Cu contents (R2=0.19). However, inasmuch as total Cu content improved the regression model showing the inhibitory effect of Cu in both bioassays, it accounted for a mere small proportion of the variance. This was despite the wide range of Cu contents in the soils studied (51-2878 mg kg-1). Hence, due to the known sensitivity of the nitrification and nitrogen mineralization process to physicochemical characteristics of soils, these bioassays seem to have limited applicability for metal toxicity assessment in metal-contaminated soils.
机译:硝化和氮矿化的微生物生物测定法已用于评估金属污染土壤的土壤质量。我们评估了硝化和氮矿化生物测定作为由金属污染引起的土壤退化的质量指标的有效性。我们根据ISO 14238(2012)和ISO 15685(2012)的协议对从智利中部农业地区收集的90种土壤样本进行了标准测试,这些样本过去曾受到采矿活动的污染。潜在的硝化速率(PNR)最好用pH和有机物含量(OM)(R2 = 0.32)来解释,而氮矿化作用(Nmin)最好用OM和粘土含量(R2 = 0.44)来解释。在生物测定的归一化之后,相对于OM的响应在PNR和pH与总Cu含量(R2 = 0.22)之间以及在Nmin和粘土与总Cu含量(R2 = 0.19)之间产生显着相关性。但是,由于总铜含量改善了回归模型,显示了两种生物测定中铜的抑制作用,因此它仅占变异的很小一部分。尽管研究的土壤中的铜含量范围很广(51-2878 mg kg-1)。因此,由于硝化和氮矿化过程对土壤理化特性的已知敏感性,这些生物测定似乎对金属污染土壤中金属毒性评估的适用性有限。

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