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Effects of Acid Mine Drainage on Calcareous Soil Characteristics and Lolium perenne L. Germination

机译:酸性矿山排水对石灰性土壤特性和黑麦草萌发的影响

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摘要

Acid mine drainage (AMD) is a serious environmental problem resulting from extensive sulfide mining activities. There is a lack of more comprehensive and detailed studies on the effect of AMD on calcareous soil characteristics and seed germination. In this study, five calcareous soil samples, collected from Xiaoyi, Taigu, Xiangning, Hejin, and Xixian counties in Shanxi Province, China, were used to investigate the effects of acid AMD on soil characteristics and Lolium perenne L. germination through laboratory culture experiments. The results showed that the increase in the total soil calcium oxide and magnesium oxide (CaO + MgO) contents led to a rise in the amount of Fe2+ in AMD converted into Fe3+, and that major ions (H+, Fe, SO42−) in AMD were trapped in the soil. The total Cao + MgO contents in the soil collected from Hejin and Taigu counties were 14.23% and 6.42%, the pH of AMD-polluted soil decreased to 7.24 and 3.10, and 98.7% and 54.0% of the Fe2+, 99.9% and 58.6% of the total Fe, and 76.0% and 26.4% of the SO42−, respectively, were trapped in the soil when the AMD volume to soil mass ratio was 10 mL/g. The results for the soil from Taigu County showed that when the soil had an AMD volume to soil mass ratio of 10 mL/g, the organic matter, available phosphorus (available P), available potassium (available K), Cr, and Cd contents in soil decreased by 16.2%, 63.0%, 97.1%, 7.8%, and 73.2%, respectively; the total phosphorus (total P) and total potassium (total K) did not significantly change; whereas the available nitrogen (available N) and total nitrogen (total N) increased to 16.1 times and 1.76 times, respectively. Compared to the initial soil collected from Taigu County, the Lolium perenne L. germination rate decreased by 81.1%, and the cumulative amount of Cr in the Lolium perenne L. increased by 7.24 times in the AMD-polluted soil when the AMD volume to soil mass ratio was 6 mL/g. The soil conditions could not support Lolium perenne L. germination when the AMD volume to soil mass ratio was 10 mL/g. The outcomes of this study could have important implication in understanding the hydrological/geochemical-behaviour of major ions of AMD in calcareous soil. The findings also have great significance in predicting plant growth behavior in AMD-polluted calcareous soil.
机译:酸性矿山排水(AMD)是由广泛的硫化物开采活动引起的严重环境问题。缺少关于AMD对钙质土壤特性和种子发芽的影响的更全面和详细的研究。在这项研究中,从中国山西孝义,太谷,向宁,河津和西县等县收集的五个钙质土壤样品,通过实验室培养实验研究了酸性AMD对土壤特性和黑麦草萌发的影响。 。结果表明,土壤总氧化钙和氧化镁(CaO + MgO)含量的增加导致AMD中的Fe 2 + 转化为Fe 3+ < / sup>,并且AMD中的主要离子(H + ,Fe,SO4 2-)被困在土壤中。从河津和太谷县收集的土壤中Cao + MgO的总含量分别为14.23%和6.42%,AMD污染土壤的pH值分别降至7.24和3.10,以及Fe 2+ <的98.7%和54.0%。 / sup>时,AMD体积与土壤质量比为10时,总Fe的99.9%和58.6%,以及SO4 2-的76.0%和26.4%被困在土壤中毫升/克太谷县土壤分析结果表明,当AMD体积与土壤质量比为10 mL / g时,有机质,有效磷(有效磷),有效钾(有效钾),Cr和Cd含量土壤中分别减少了16.2%,63.0%,97.1%,7.8%和73.2%;总磷(总磷)和总钾(总钾)没有显着变化;而有效氮(有效氮)和总氮(总氮)分别增加到16.1倍和1.76倍。与原始太谷县土壤相比,黑麦草发芽率降低了81.1%,当AMD污染土壤时,黑麦草中Cr的累积量在AMD污染土壤中增加了7.24倍。质量比为6mL / g。当AMD体积与土壤质量比为10 mL / g时,土壤条件不能支持黑麦草的发芽。这项研究的结果可能对了解钙质土壤中AMD主要离子的水文/地球化学行为具有重要意义。这些发现对于预测AMD污染的钙质土壤中的植物生长行为也具有重要意义。

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