首页> 外文期刊>Journal of Hydrology >Sources and processes of contaminant loss from an intensively grazed catchment inferred from patterns in discharge and concentration of thirteen analytes using high intensity sampling
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Sources and processes of contaminant loss from an intensively grazed catchment inferred from patterns in discharge and concentration of thirteen analytes using high intensity sampling

机译:使用高强度采样从密集放牧的集水区的污染物流失的来源和过程,这些流失是根据排放和浓缩十三种分析物的模式得出的

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Contaminants in water from intensively grazed catchments have been shown to cause significant environmental impacts. Effective intervention to reduce contaminant loads depends on identifying their sources and processes of mobilisation and transport. In this study, flow (Q) and analyte concentrations (CA) from a 12 ha catchment in north-west Tasmania used for grazing dairy cattle were monitored at a fine temporal scale and used to infer sources and processes of loss. Three groups of analytes identified based on CA–Q relationships, which included hysteresis loops, demonstrated that the TP group (TP, DRP, TSS, TN, E. coli and Enterococcus) was transported by surface runoff processes while the behaviour of the NO3 group (NO3, TDS, Ca, Mg, Na) was explained by subsurface processes and pathways. The NH4 group (NH4, K) was dominated by the addition of large quantities of analyte from grazing. In addition to the CA–Q relationships, concentrations of most analytes decreased linearly over each season of runoff. NH4 and K concentrations decreased exponentially following grazing events while TP concentrations decreased linearly. The study demonstrated the importance of understanding surface water and groundwater interactions and that relationships between runoff events, analyte concentrations and management as revealed by a fine temporal sampling regime may yield significant insights to sources and processes of loss of analytes in surface flow, at a given scale.
机译:密集放牧的流域水中的污染物已显示出对环境的重大影响。减少污染物负荷的有效干预措施取决于确定其来源以及动员和运输的过程。在这项研究中,塔斯马尼亚西北部一个12公顷流域用于放牧奶牛的流量(Q)和分析物浓度(CA)在良好的时间尺度上进行了监测,并用于推断损失的来源和过程。根据CA-Q关系确定的三组分析物(包括磁滞回线)表明,TP组(TP,DRP,TSS,TN,大肠杆菌和肠球菌)通过地表径流过程运输,而NO3组的行为(NO3,TDS,Ca,Mg,Na)通过地下过程和途径来解释。 NH4组(NH4,K)以放牧中添加的大量分析物为主导。除了CA-Q关系之外,大多数分析物的浓度在每个径流季节都呈线性下降。放牧事件后,NH4和K的浓度呈指数下降,而TP的浓度呈线性下降。这项研究证明了了解地表水和地下水相互作用的重要性,并且在一个给定的时间采样机制下,径流事件,分析物浓度和管理之间的关系可以在给定的条件下提供对地表水分析物损失的来源和过程的深刻见解。规模。

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