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Arsenic Dynamics in Porewater of an Intermittently Irrigated Paddy Reid in Bangladesh

机译:孟加拉国间歇灌溉稻田里德的废水中砷动力学

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摘要

In Bangladesh, irrigation of dry season rice (bora) with arsenic-contaminated groundwater is leading to increased As levels in soils and rice, and to concerns about As-induced yield reduction. Arsenic concentrations and speciation in soil porewater are strongly influenced by redox conditions, and thus by water management during rice growth. We studied the dynamics of As, Fe, P, Si, and other elements in porewater of a paddy field near Sreenagar (Munshiganj), irrigated according to local practice, in which flooding was intermittent During early rice growth, As porewater concentrations reached up to 500 μg L ~(-1) and were dominated by As~(111), but As release was constrained to the lower portion of the soil above the plow pan. In the later part of the season, soil conditions were oxic throughout the depth range relevant to rice roots and porewater concentrations only intermittently increased to ~150 μg L~(-1) As~V following irrigation events. Our findings suggest that intermittent irrigation, currently advocated in Bangladesh for water-saving purposes, may be a promising means of reducing As input to paddy soils and rice plant exposure to As.
机译:在孟加拉国,用砷污染的地下水灌溉旱季稻米会导致土壤和稻米中砷的含量增加,并引起人们对砷导致的减产的担忧。土壤孔隙水中的砷浓度和形态受氧化还原条件的影响很大,因此也受水稻生长过程中水分管理的影响。我们研究了Sreenagar(Munshiganj)附近稻田的孔隙水中As,Fe,P,Si等元素的动态,并根据当地的实践进行了灌溉,在水稻早期生长过程中,断断续续地发生洪水,当孔隙水浓度达到500μgL〜(-1)且以As〜(111)为主,但As的释放被限制在犁盘上方土壤的下部。在该季节的后期,土壤条件在与稻根相关的整个深度范围内都是有氧的,并且在灌溉事件之后,孔隙水浓度仅间歇性增加至〜150μgL〜(-1)As〜V。我们的研究结果表明,目前孟加拉国出于节水目的而倡导的间歇灌溉可能是减少稻田土壤和水稻植物接触砷的砷的一种有前途的手段。

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  • 来源
    《Environmental Science & Technology》 |2011年第3期|p.971-976|共6页
  • 作者单位

    Eawag, Swiss Federal Institute of Aquatic Science and Technology, Ueberlandstrasse 133, CH-SBOO Duebendorf, Switzerland,Institute of Biogeochemistry and Pollutant Dynamics, Department of Environmental Sciences, ETH Zurich, CH-8092 Zurich, Switzerland;

    rnEawag, Swiss Federal Institute of Aquatic Science and Technology, Ueberlandstrasse 133, CH-SBOO Duebendorf, Switzerland;

    rnEawag, Swiss Federal Institute of Aquatic Science and Technology, Ueberlandstrasse 133, CH-SBOO Duebendorf, Switzerland;

    rnInstitute of Biogeochemistry and Pollutant Dynamics, Department of Environmental Sciences, ETH Zurich, CH-8092 Zurich, Switzerland,Department of Environmental Earth System Science, Stanford University, Stanford, California 94305;

    rnInstitute of Biogeochemistry and Pollutant Dynamics, Department of Environmental Sciences, ETH Zurich, CH-8092 Zurich, Switzerland;

    rnInstitute of Biogeochemistry and Pollutant Dynamics, Department of Environmental Sciences, ETH Zurich, CH-8092 Zurich, Switzerland;

    rnDepartment of Civil Engineering, Dhaka University of Engineering and Technology, Gazipur-1700, Bangladesh;

    rnDepartment of Civil Engineering, Bangladesh University of Engineering and Technology, Dhaka-1000, Bangladesh;

    rnDepartment of Civil Engineering, Bangladesh University of Engineering and Technology, Dhaka-1000, Bangladesh;

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