Item talk:Q239264
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{
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Soil water in the top 10\u00a0cm was significantly affected by both evaporation and infiltration. Water at 10\u201340\u00a0cm depth in the grassland and arable land, and 10\u201360\u00a0cm in poplar forest, showed a relatively short residence time, as a substantial proportion of antecedent soil water was mixed with a 92-mm storm infiltration event, whereas below those depths (down to 150\u00a0cm), depleted \u03b418O spikes suggested that some storm water bypassed the shallow soil layers. Significant differences, in soil-water content and \u03b418O values, within a small area, suggested that the proportion of immobile soil water and water flowing in subsurface pathways varies depending on local vegetation cover, soil characteristics and irrigation applications. Soil-water \u03b418O values revealed that preferential flow and diffuse flow coexist. Preferential flow was active within the root zone, independent of antecedent soil-water content, in both poplar forest and arable land, whereas diffuse flow was observed in grassland. The depleted \u03b418O spikes at 20\u201350\u00a0cm depth in the arable land suggested the infiltration of irrigation water during the dry season. Temporal isotopic variations in precipitation were subdued in the shallow groundwater, suggesting more complete mixing of different input waters in the unsaturated zone before reaching the shallow groundwater.", "description": "14 p. 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