首页> 外文会议>International Mine Water Association Symposium >Quantification of Acidity Deposition in the Sediment of a former lignite mining lake in the Wackersdorf Mining District (Eastern Bavaria)
【24h】

Quantification of Acidity Deposition in the Sediment of a former lignite mining lake in the Wackersdorf Mining District (Eastern Bavaria)

机译:瓦克索夫矿区(巴伐利亚东部)前褐煤矿湖泥沙沉积物的定量

获取原文

摘要

From 1982 to 2001 acidic conditions prevailed at former lignite mining Lake Knappensee. Since 2001 the acidity of the lake water continuously decreased reaching circum-neutral pH conditions in 2010.Based on acidity time series of the lake water in combination with water budgets derived from a regional groundwater model the cumulative acidity loss in the lake for the time span from 2001 to 2015 can be estimated to be 8400 kmol.Internal neutralization by biogenic sulfate reduction with consecutive deposition of reduced sulfur in the lake sediment was supposed to be the crucial process leading to the observed decrease in lake water acidity. In order to test this hypothesis elaborate quantitative field and laboratory investigations were launched in December 2014.15 sediment cores distributed over the lake's area were sampled and analyzed for reduced sulfur species at the hydrological laboratory of the University of Bayreuth. The measured sulfur contents were converted into deposited proton equivalents and finally the results were extrapolated for the total lake sediment.The amount of at least 6400 kmol of acidity deposited and fixed in the lake sediments estimated with this procedure compares well to the acidity-loss of 8400 kmol which was calculated for the lake water as mentioned above.Measurements and data evaluation allowed for identification of naturally occurring internal neutralization to be the major process for the observed acidity decrease in the lake water. The internal neutralization processes are not only beneficial to the lake water quality, but are also of great practical importance for the assessment of the hydrochemical state of the lake.The methodology applied to Lake Knappensee consisting of field scale sediment investigations combined with water budgets gained from regional groundwater modeling could also be used for the assessment of the hydrochemical state of other mining lakes.
机译:从1982年到2001年,前褐煤矿湖克拉帕德湖占酸性条件。自2001年以来,2010年湖水的酸度持续降低达到环中性pH条件。基于湖水的酸度时间序列,与区域地下水模型的水预算结合在湖泊中占湖泊的累积酸度损失从2001年到2015年,可以估计为8400 kmol.Enternic硫酸盐随着湖泊沉积物中连续沉积的生物硫酸盐降低,应该是导致湖水酸度下降的关键方法。为了测试这一假设,精心制定的定量领域和实验室调查于2014年12月推出.15分布在湖区地区的沉积物核心被取样,并分析了拜罗伊大学水文实验室的硫种类。将测定的硫含量转化为沉积的质子等效物,最后将结果推断为总湖泊沉积物。沉积和固定在湖泊沉积物中的至少6400厘米的酸度的量​​与酸度损失相比如上所述,为湖水计算的8400 kmol.Reasurese和数据评估允许鉴定天然存在的内部中和,是湖水中观察到的酸度降低的主要过程。内部中和过程不仅有利于湖水质量,而且对湖的水化学状态的评估也是很大的实际重要性。应用于Knappensee湖的方法,包括野外沉积物调查,结合来自水预算的水预算区域地下水建模也可用于评估其他采矿湖泊的水化学状态。

著录项

相似文献

  • 外文文献
  • 中文文献
  • 专利
获取原文

客服邮箱:kefu@zhangqiaokeyan.com

京公网安备:11010802029741号 ICP备案号:京ICP备15016152号-6 六维联合信息科技 (北京) 有限公司©版权所有
  • 客服微信

  • 服务号