首页> 外文期刊>Environmental Toxicology and Chemistry >SOIL PROPERTIES AFFECTING THE TOXICITY OF CuCl2 AND NiCl2 FOR SOIL MICROBIAL PROCESSES IN FRESHLY SPIKED SOILS
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SOIL PROPERTIES AFFECTING THE TOXICITY OF CuCl2 AND NiCl2 FOR SOIL MICROBIAL PROCESSES IN FRESHLY SPIKED SOILS

机译:影响新鲜土壤中CuCl2和NiCl2对土壤微生物过程毒性的土壤性质

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It generally is unknown to what extent the toxicity of Cu and Ni for soil microbial processes varies among different soils. A comparative study was made using three different microbial assays (nitrification potential, glucose-induced respiration, and C-mineralization of a plant residue) in 19 (for Cu) or 16 (for Ni) soils with contrasting soil properties. Each soil was spiked with CuCl2 or NiCl2 at seven different concentrations, and the bioassays were started after a 7-d equilibration period. The Cu and Ni toxicity thresholds varied 19- to 90-fold among soils. The differences in both Cu and Ni toxicity among soils were neither explained by soil solution metal concentrations nor by free ion activities calculated from soil solution composition. Copper toxicity thresholds (total concentrations) increased with increasing organic matter content or cation exchange capacity (CEC) and, surprisingly, decreased with increasing pH depending on the assay. Nickel toxicity thresholds consistently increased with increasing CEC, background Ni, and clay content for all three assays. Thresholds expressed as soil solution free ion activities all significantly decreased with increasing soil solution pH (r2 = 0.57–0.93), consistent with a decreased H+:M2+ competition at the biological membrane. That competition largely counteracts the H+:M2+ competition for sorption, effectively explaining the insignificant or weak effect of pH on total Ni or Cu toxicity thresholds. It is concluded that free metal-ion activity alone does not explain variation in metal toxicity among soils.
机译:通常未知的是,Cu和Ni对土壤微生物过程的毒性在不同土壤中变化的程度。在19种(铜)或16种(镍)土壤中使用三种不同的微生物测定法(硝化潜能,葡萄糖诱导的呼吸作用和植物残渣的C矿化)进行了比较研究,具有不同的土壤特性。在每种土壤中掺入7种不同浓度的CuCl2或NiCl2,并在7天的平衡期后开始生物测定。在土壤中,铜和镍的毒性阈值变化19到90倍。土壤中铜和镍的毒性差异既不能通过土壤溶液中的金属浓度来解释,也不能通过根据土壤溶液成分计算出的自由离子活性来解释。铜毒性阈值(总浓度)随有机物含量或阳离子交换容量(CEC)的增加而增加,令人惊讶的是,根据测定法,铜的毒性阈值随pH的增加而降低。对于所有三种测定,镍毒性阈值均随着CEC,背景镍和粘土含量的增加而持续增加。阈值表示为土壤溶液的自由离子活性,随着土壤溶液pH值的增加(r2 = 0.57–0.93)而显着降低,这与生物膜上H +:M2 +竞争的降低相一致。这种竞争在很大程度上抵消了H +:M2 +的吸附竞争,有效地解释了pH值对总Ni或Cu毒性阈值的影响微不足道。结论是,仅游离金属离子活性不能解释土壤间金属毒性的变化。

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