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Acidification of floodplains due to river level decline during drought

机译:干旱期间河平面下降导致洪泛区酸化

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摘要

A severe drought from 2007 to 2010 resulted in the lowest river levels (1.75 m decline from average) in over 90 years of records at the end of the Murray-Darling Basin in South Australia. Due to the low river level and inability to apply irrigation, the groundwater depth on the adjacent agricultural flood plain also declined substantially (1-1.5 m) and the alluvial clay subsoils dried and cracked. Sulfidic material (pH > 4, predominantly in the form of pyrite, FeS_2) in these subsoils oxidised to form sulfuric material (pH < 4) over an estimated 3300 ha on 13 floodplains. Much of the acidity in the deeply cracked contaminated soil layers was in available form (in pore water and on cation exchange sites), with some layers having retained acidity (iron oxyhydroxysulfate mineral jarosite). Post drought, the rapid raising of surface and ground water levels mobilised acidity in acid sulfate soil profiles to the floodplain drainage channels and this was transported back to the river via pumping. The drainage water exhibited low pH (2-5) with high soluble metal (Al, Co, Mn, Fe, Mn, Ni, and Zn) concentrations, in exceedance of guidelines for ecosystem protection. Irrigation increased the short-term transport of acidity, however loads were generally greater in the non-irrigation (winter) season when rainfall is highest (0.0026 tonnes acidity/ha/day) than in the irrigation (spring-summer) season (0.0013 tonnes acidity/ha/day). Measured reductions in groundwater acidity and increases in pH have been observed over time but severe acidification persisted in floodplain sediments and waters for over two years post-drought Results from 2-dimensional modelling of the river-floodplain hydrological processes were consistent with field measurements during the drying phase and illustrated how the declining river levels led to floodplain acidification. A modelled management scenario demonstrated how river level stabilisation and limited irrigation could have prevented, or greatly lessened the severity of the acidification.
机译:从2007年到2010年的严重干旱,导致南澳大利亚默里-达令盆地尽头的90多年以来最低的河流水位(较平均水平下降175万)。由于河水位低和无法灌溉,相邻农业洪泛平原的地下水深度也大幅下降(1-1.5 m),冲积粘土地基干燥并开裂。这些底土中的硫化物(pH> 4,主要为黄铁矿,FeS_2形式)在13个洪泛区上约3300公顷上氧化形成硫化物(pH <4)。深度开裂的受污染土壤层中的大部分酸度都是可用的形式(在孔隙水和阳离子交换位点),有些层保留了酸度(羟基羟基硫酸铁矿物黄钾铁矾)。干旱后,地表水和地下水位的迅速升高将酸性硫酸盐土壤剖面中的酸度转移至洪泛区排水渠,并通过抽水运回河中。排泄水的pH值较低(2-5),且可溶性金属(Al,Co,Mn,Fe,Mn,Ni和Zn)的浓度较高,超出了生态系统保护的准则。灌溉增加了酸度的短期输送,但是在降雨量最高(0.0026吨酸度/公顷/天)的非灌溉(冬季)季节,其负荷通常大于灌溉(春夏季)的负荷(0.0013吨)酸度/公顷/天)。观察到随着时间的推移,已测得的地下水酸度降低和pH值升高,但在干旱后两年多的时间里,洪泛区沉积物和水域仍持续发生严重的酸化作用。二维河洪平原水文过程的模拟结果与实测值一致。干燥阶段,并说明了河流水位下降如何导致洪泛区酸化。一个模型化的管理方案表明,河流水位稳定和有限的灌溉本来可以防止或大大降低酸化的严重性。

著录项

  • 来源
    《Journal of Contaminant Hydrology》 |2014年第6期|10-23|共14页
  • 作者单位

    Environment Protection Authority (South Australia), GPO Box 2607, Adelaide, SA 5001, Australia ,CSIRO Land and Water, Private Bag No. 2, Glen Osmond, SA 5064, Australia ,Acid Sulfate Soils Centre, The University of Adelaide, SA 5005, Australia;

    Environment Protection Authority (South Australia), GPO Box 2607, Adelaide, SA 5001, Australia;

    Environment Protection Authority (South Australia), GPO Box 2607, Adelaide, SA 5001, Australia;

    Freeman Cook and Associates Ltd, PO Box 97, Glasshouse Mountains Q4518, Queensland, Australia;

    Environment Protection Authority (South Australia), GPO Box 2607, Adelaide, SA 5001, Australia;

    CSIRO Land and Water, Private Bag No. 2, Glen Osmond, SA 5064, Australia ,Acid Sulfate Soils Centre, The University of Adelaide, SA 5005, Australia ,School of the Environment, Flinders University, PO Box 2100, Adelaide, SA 5001, Australia;

    CSIRO Land and Water, Private Bag No. 2, Glen Osmond, SA 5064, Australia;

    CSIRO Land and Water, Private Bag No. 2, Glen Osmond, SA 5064, Australia ,Acid Sulfate Soils Centre, The University of Adelaide, SA 5005, Australia;

  • 收录信息 美国《科学引文索引》(SCI);美国《工程索引》(EI);美国《生物学医学文摘》(MEDLINE);美国《化学文摘》(CA);
  • 原文格式 PDF
  • 正文语种 eng
  • 中图分类
  • 关键词

    Pyrite oxidation; Acid sulfate soils; Acid drainage; Surface-groundwater interactions; Climate change;

    机译:黄铁矿氧化;酸性硫酸盐土壤;排酸地表-地下水相互作用;气候变化;

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