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Major and trace elements of selected pedons in the USA 总被引:6,自引:0,他引:6
Few studies of soil geochemistry over large geographic areas exist, especially studies encompassing data from major pedogenic horizons that evaluate both native concentrations of elements and anthropogenically contaminated soils. In this study, pedons (n = 486) were analyzed for trace (Cd, Co, Cr, Cu, Hg, Mn, Ni, Pb, Zn) and major (Al, Ca, Fe, K, Mg, Na, P, Si, Ti, Zr) elements, as well as other soil properties. The objectives were to (i) determine the concentration range of selected elements in a variety of U.S. soils with and without known anthropogenic additions, (ii) illustrate the association of elemental source and content by assessing trace elemental content for several selected pedons, and (iii) evaluate relationships among and between elements and other soil properties. Trace element concentrations in the non-anthropogenic dataset (NAD) were in the order Mn > (Zn, Cr, Ni, Cu) > (Pb, Co) > (Cd, Hg), with greatest mean total concentrations for the Andisol order. Geometric means by horizon indicate that trace elements are concentrated in surface and/or B horizons over C horizons. Median values for trace elements are significantly higher in surface horizons of the anthropogenic dataset (AD) over the NAD. Total Al, Fe, cation exchange capacity (CEC), organic C, pH, and clay exhibit significant correlations (0.56, 0.74, 0.50, 0.31, 0.16, and 0.30, respectively) with total trace element concentrations of all horizons of the NAD. Manganese shows the best inter-element correlation (0.33) with these associated total concentrations. Total Fe has one of the strongest relationships, explaining 55 and 30% of the variation in total trace element concentrations for all horizons in the NAD and AD, respectively. 相似文献
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Thomas C. Winter 《Journal of the American Water Resources Association》2000,36(2):305-311
ABSTRACT: The vulnerability of wetlands to changes in climate depends on their position within hydrologic landscapes. Hydrologic landscapes are defined by the flow characteristics of ground water and surface water and by the interaction of atmospheric water, surface water, and ground water for any given locality or region. Six general hydrologic landscapes are defined; mountainous, plateau and high plain, broad basins of interior drainage, riverine, flat coastal, and hummocky glacial and dune. Assessment of these landscapes indicate that the vulnerability of all wetlands to climate change fall between two extremes: those dependent primarily on precipitation for their water supply are highly vulnerable, and those dependent primarily on discharge from regional ground water flow systems are the least vulnerable, because of the great buffering capacity of large ground water flow systems to climate change. 相似文献
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In Brazil most Construction and Demolition Waste (C&D waste) is not recycled. This situation is expected to change significantly, since new federal regulations oblige municipalities to create and implement sustainable C&D waste management plans which assign an important role to recycling activities. The recycling organizational network and its flows and components are fundamental to C&D waste recycling feasibility. Organizational networks, flows and components involve reverse logistics. The aim of this work is to introduce the concepts of reverse logistics and reverse distribution channel networks and to study the Brazilian C&D waste case. 相似文献
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累托石对水中染料碱性桃红的吸附 总被引:1,自引:0,他引:1
采用累托石作为水中碱性桃红的吸附剂.考察了振荡时间、pH值、累托石用量、碱性桃红初始浓度等因素对吸附效果的影响.测定了吸附等温线,对吸附动力学规律进行了数学模拟.结果表明,振荡时间、累托石用量、碱性桃红初始浓度等因素对吸附效果有重要影响.对于初始质量浓度为50 mg/L的碱性桃红水溶液,最适宜吸附条件为:振荡时间30 min,累托石用量200 mg/100 mL,pH值为6.累托石对水中碱性桃红的吸附等温线呈"S"型,等温吸附规律可用Freundlich模式较好地描述,吸附动力学规律可用Bangham公式模拟. 相似文献
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农业非点源污染田间模型及其应用 总被引:3,自引:4,他引:3
非点源污染的负荷定量化研究是控制、评价和管理非点源污染的基础.农业非点源污染负荷估算包括农田排水估算和排水中的污染物浓度预测2个环节.依据水量平衡原理,农田排水应用DRAINMOD模型估算;将农田的施肥和灌溉过程"合成"作为田间污染物浓度的脉冲输入,农田排水中的污染物浓度变化则视作对应于此脉冲输入的响应过程,而污染物在田间的复杂迁移转化过程以逆高斯概率密度函数隐含表达.以此为基础,构建了农田尺度农业非点源污染负荷估算模型.以青铜峡灌区典型试验区为例,对稻田排水沟中硝态氮(NO_3~--N)和总磷(TP)的负荷过程进行了模拟,结果表明,模型估算结果和实测污染物负荷过程非常接近,Nash-Suttcliffe模拟效率系数分别为0.963和0.945,表明该模型具有较高的可靠性. 相似文献
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