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DISCREPANCY OF THE MICROBIAL RESPONSE TO ELEVATED COPPER BETWEEN FRESHLY SPIKED AND LONG-TERM CONTAMINATED SOILS

机译:新鲜和长期污染土壤中铜对微生物响应的差异

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A systematic comparison of Cu toxicity thresholds was made between freshly spiked soils and soils in which elevated Cu concentrations have been present for various times. Three uncontaminated soils were spiked and experimentally leached or incubated outdoors for up to 18 months. Additionally, five field-contaminated soils with a 6- to 80-year-old Cu contamination were sampled, and corresponding uncontaminated soils were spiked to identical total concentrations. All soil samples were subjected to three microbial assays (nitrification potential, glucose-induced respiration, and maize residue C-mineralization). Experimental leaching or soil incubation after spiking reduced Cu toxicity (1.3- or 2.3-fold increase of dose, respectively, to inhibit process by 50% [ED50]). No significant effects of soil type, aging time (6, 12, or 18 months), or bioassay on the factor change of ED50 were found. Significant reductions of microbial activity in field-contaminated soils were only identified in 2 of the 15 series (three assays in five soils), whereas freshly spiking the corresponding control soils significantly affected these processes in 12 series. Soil solution Cu concentrations significantly decreased on leaching at corresponding total soil Cu, and smaller decreases were found during additional aging. Soil solution Cu concentrations largely explain changes in Cu toxicity on leaching and aging, although additional variation may be related to changes in the sensitivity of microbial populations. It is concluded that total Cu toxicity thresholds are lower in freshly spiked soils compared to soils in which Cu salts have equilibrated and leaching has removed excess soluble salts. The large variability of soil microbial processes creates a large uncertainty about the magnitude of the factor by which aging mitigates Cu toxicity.
机译:在新鲜加标土壤和不同时间出现高浓度Cu的土壤之间进行了Cu毒性阈值的系统比较。将三种未污染的土壤加标,并通过实验浸出或在户外孵育长达18个月。此外,还对5种具有6至80年历史的Cu污染的田间污染土壤进行了采样,并将相应的未污染土壤加标至相同的总浓度。所有土壤样品均经过了三种微生物测定(硝化潜力,葡萄糖诱导的呼吸作用和玉米残留碳矿化)。加标后的实验浸出或土壤培养降低了铜的毒性(剂量分别增加了1.3倍或2.3倍,以使过程抑制50%[ED50])。没有发现土壤类型,老化时间(6、12或18个月)或生物测定对ED50因子变化的显着影响。仅在15个系列中的2个中发现了被田地污染的土壤中微生物活性的显着降低(在5个土壤中进行了3种测定),而在12个系列中,新加标相应的对照土壤会明显影响这些过程。在相应的总土壤铜浸出后,土壤溶液中铜的浓度显着降低,而在额外的老化过程中,发现的降低幅度较小。土壤溶液中铜的浓度很大程度上解释了浸出和老化后铜毒性的变化,尽管其他变化可能与微生物种群敏感性的变化有关。结论是,与铜盐平衡且浸出已去除过量可溶性盐的土壤相比,新鲜加标土壤中的总铜毒性阈值较低。土壤微生物过程的巨大变异性对老化减轻铜毒性的因素的幅度产生了很大的不确定性。

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