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The variation and controls of mean transit times in Australian headwater catchments

机译:澳大利亚散水集水区的平均途中的变化与控制

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Determining mean transit times in headwater catchments is critical for understanding catchment functioning and understanding their responses to changes in landuse or climate. Determining whether mean transit times (MTTs) correlate with drainage density, slope angle, area, or land cover permits a better understanding of the controls on water flow through catchments and allows first-order predictions of MTTs in other catchments to be made. This study assesses whether there are identifiable controls on MTTs determined using(3)H in headwater catchments of southeast Australia. Despite MTTs at baseflow varying from a few years to 100 years, it was difficult to predict MTTs using single or groups of readily-measured catchment attributes. The lack of readily-identifiable correlations hampers the prediction of MTTs in adjacent catchments even where these have similar geology, land use, and topography. The long MTTs of the Australian headwater catchments are probably in part due to the catchments having high storage volumes in deeply-weathered regolith, combined with low recharge rates due to high evapotranspiration. However, the difficulty in estimating storage volumes at the catchment scale hampers the use of this parameter to estimate MTTs. The runoff coefficient (the fraction of rainfall exported via the stream) is probably also controlled by evapotranspiration and recharge rates. Correlations between the runoff coefficient and MTTs in individual catchments allow predictions of MTTs in nearby catchments to be made. MTTs are shorter in high rainfall periods as the catchments wet up and shallow water stores are mobilized. Despite the contribution of younger water, the major ion geochemistry in individual catchments commonly does not correlate with MTTs, probably reflecting heterogeneous reactions and varying degrees of evapotranspiration. Documenting MTTs in catchments with high storage volumes and/or low recharge rates elsewhere is important for understanding MTTs in diverse environments.
机译:确定沿着地水集液中的平均运输时间对于了解集水功能和理解其对土地使用或气候变化的反应至关重要。确定是否与排水密度,斜角,面积或陆盖相关的平均传递时间(MTTS)允许更好地了解水流通过集水流动的控制,并允许在其他集水区中进行MTTS的一阶预测。本研究评估是否在澳大利亚东南部地区使用(3)H确定的MTTS上有可识别的控制。尽管从几年的基础变化到> 100年时,尽管MTTS变化,但难以使用单一或一组易测测量的集水属性预测MTTS。缺乏易于识别的相关性妨碍了甚至在这些具有类似地质,土地利用和地形中的相邻集水区中的MTTS的预测。澳大利亚地区的长期MTTS可能部分是由于具有高储存量的高存储体积,而由于高蒸发而与低充电率相结合。然而,难以在集距量表中估计存储体积的存储体积妨碍使用该参数来估计MTT。径流系数(通过流导出的降雨分数)也可能通过蒸发和充电率来控制。单个集水区中的径流系数和MTT之间的相关性允许在附近的集水区内预测MTT。随着集水器湿润和浅水储存的流量,MTTS在高降雨期间短。尽管较年轻的水贡献,但各个流域的主要离子地球化学通常与MTTS不相关,可能反映异质反应和不同程度的蒸散。记录在具有高存储卷的集水区中的MTT和/或其他地方的低电平速率对于在不同环境中的理解MTT而言非常重要。

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