首页> 外文期刊>Canadian Journal of Soil Science >Long-term solute redistribution in relation to landscape morphology and soil distribution in a variable glacial till landscape
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Long-term solute redistribution in relation to landscape morphology and soil distribution in a variable glacial till landscape

机译:与可变冰川耕地景观相关的景观形态和土壤分布的长期溶质再分配

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Landscape delineation based on soilslope associations with similar patterns of solute redistribution would allow for better agro-environmental land management. Long-term redistribution of solutes was examined in relation to topographic variables and static soil properties in a glacial till landscape near Miniota, Manitoba. Static soil properties that were the best predictors of solute redistribution included CO_3, Ahor, Solum and OrgC. Temporal variability overshadowed the influence of topographic variables and static soil properties on dynamic solute redistribution within the crop rooting zone (i.e., 120 cm). Topographic variables (relative elevation, topographic index, contributing area) and static soil properties (A horizon depth, solum depth, Ahorizon organic carbon) were correlated to SO_4~(2-) and NO_3~- redistribution. An unexpected result was that more statistically significant relationships were found between these parameters and solute redistribution below 120 cm rather than within the root zone. Very low NO_3~- concentrations were found in the rooting zone at most sample positions, indicating that crop demand during recent growing seasons matched or exceeded supply. Accumulations of NO_3~- below the rooting zone indicated that deep percolation of NO_3~- has been an important process over the longer term throughout the upper and mid slope positions of this landscape. A lack of NO_3~- accumulation in one lower-toe position and the depression indicated that excess NO_3~- in these profiles may have been leached into the groundwater and/or removed via denitrification or simply may not have accumulated. There appears to be utility in using static soil properties and topographic variables as indicators of dynamic processes of solute redistribution, however, a priori knowledge of soil-landscape relationships and an understanding of associated pedogenic processes and hydrologie regimes are required to achieve sensible results.
机译:基于具有相似溶质再分配模式的土壤坡关联的景观描述将有助于更好的农业环境土地管理。在马尼托巴省Miniota附近的冰川耕地景观中,研究了与地形变量和静态土壤性质相关的溶质的长期再分布。静态土壤特性是溶质再分配的最佳预测因子,包括CO_3,Ahor,Solum和OrgC。时间变化掩盖了地形变量和静态土壤特性对作物生根区(即120 cm)内动态溶质再分配的影响。地形变量(相对海拔,地形指数,贡献面积)和静态土壤特性(地平线深度,贫民窟深度,阿霍里宗有机碳)与SO_4〜(2-)和NO_3〜-重新分布相关。出乎意料的结果是,在这些参数与120 cm以下而不是根部区域内的溶质重新分布之间发现了更具统计意义的显着关系。在大多数采样点的生根区发现NO_3〜-浓度很低,表明最近生长期的农作物需求与供应相匹配或超过供应。在生根区以下的NO_3〜-的积累表明,从长远来看,NO_3〜-的深度渗入一直是该景观上坡和中坡位置的重要过程。在一个较低的脚趾位置缺少NO_3〜-的积聚和凹陷表明这些剖面中过量的NO_3〜-可能已经渗入地下水和/或通过反硝化去除或根本就没有积聚。在使用静态土壤性质和地形变量作为溶质再分布动态过程的指标方面似乎很有用,但是,要获得合理的结果,就需要先了解土壤与景观的关系,并了解相关的成岩过程和水文状况。

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