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盐渍化灌区耕荒地间水盐均衡试验分析

est Estimation of Soil Water and Salt between Irrigated Field and Adjacent saline land in Salinization District

中文摘要英文摘要

?该文以内蒙古河套灌区为背景展开田间耕荒地水盐运移规律研究。在田间试验基础上,分析作物生育期耕荒地土壤水盐的运移机理,利用水均衡模型对耕荒地土壤水的迁移规律及水收支进行了模拟分析。利用盐分收支模型计算耕荒地的盐分累积量。结果表明,作物生育灌溉期间耕地和盐碱地的水分收支基本是平衡的。定量的确认了耕地的一部分灌溉水量通过地下水渗透侧向补给邻接盐荒地,被盐荒地蒸发所消耗。此期间耕地和盐荒地都是处于积盐状态,耕地累积盐分74g/m2,盐荒地累积盐分400g/m2。荒地做为灌区盐分的贮存地,是灌区水盐平衡的重要调节因素,对干旱灌区水盐动态的研究具有重要意义。

In this study water and salt transport were studied in the irrigated field and uncultivated land of Hetao Irrigation District in Inner Mongolia province. Based on field experiments, Water and salt transport mechanism of the irrigated field and uncultivated land was analyzed in the irrigation district. Meanwhile, water and salt transport dynamics and salt accumulations were simulated with water balance and salt balance model, receptively. Results show that the input/output of water and salt of field and uncultivated land were balanced approximately in growth season. There was irrigation water was transported to adjacent uncultivated land through lateral groundwater recharge, and then the water was consumed by evapotranspiration. The salt accumulation process was both occurring during crop growth season. Salt accumulation of irrigated field and uncultivated land was 74 g/m2 and 400 g/m2, respectively. Consequently, the uncultivated land in the irrigation district was an important factor in water/salt balance progress as salt storage area. It is significent to water and salt dynamic research in arid area.

张义强、刘霞、夏玉红、王丽萍、张圣微

农业科学研究农田水利工程

农业灌溉盐荒地灌溉水入渗地下水补给水盐均衡

gricultural irrigationSaline landIrrigation water infiltrationGroundwater rechargeWater-salt balance??

张义强,刘霞,夏玉红,王丽萍,张圣微.盐渍化灌区耕荒地间水盐均衡试验分析[EB/OL].(2014-01-20)[2025-08-16].http://www.paper.edu.cn/releasepaper/content/201401-856.点此复制

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