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Water and sediment runoff and soil moisture response to grass cover in sloping citrus land, Southern China

机译:中国南方柑橘土地草盖的水和泥沙径流和土壤水分反应

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Soil erosion is recognized as one of the major environmental problems in the hilly red soil region of Jiangxi province, southern China. An eight-year field experiment was conducted to evaluate the effects of grass cover in the sloping citrus land on water and sediment runoff. Soil moisture regimes were also analysed based on the in-situ soil moisture measurement. Four treatments were carried out in the runoff plot experiment: (1) no vegetation, bare land (BL); (2) conventional treatment, citrus without grass cover (CK); (3) citrus with strip planting of Bermuda grass (SP); (4) citrus with full cover of Bermuda grass (FC). Results showed that the annual runoff volumes were significantly (P 0.05) reduced using SP (27.2 mm) and FC (33.0 mm) compared with CK (311.4 mm) and BL (456.7 mm) treatments. The SP and FC treatments significantly (P 0.05) reduced the annual average sediment yield by as much as 99.38% to 99.67%, compared with CK treatment. Soil moisture variations at the four depths (0-10, 10-20, 20-30, and 30-40 cm) were consistent with the seasonal precipitation patterns. Within the soil profile, soil moisture content increased with depth. In 3 of the 4 depths, the soil moisture contents of SP (21.20-27.84 m(3)/m(3), mean value) were the highest. Soil moisture contents of FC (14.92-26.30 m(3)/m(3), mean value) were lower than in SP because of the water consumption by plant transpiration, but were still higher than those of CK (16.03-25.00 m(3)/m(3), mean value). Based on Richards' equation numerical model, optimization tool and observed soil moisture data, actual evapotranspiration was calculated, and water balance analysis was carried out during drought and rain periods. The results indicated that planting grass in sloping citrus land can effectively reduce surface water runoff and soil erosion and increase water infiltration, but the risk of drought, resulting from planting grass, should be noticed. Compared with FC, the drought risk of SP was much lower during the drought period, and SP contributed to storage of more water in the root zone during the rain period. In conclusion, SP was a recommendable treatment.
机译:土壤侵蚀被认为是江西省南方省丘陵红土区的主要环境问题之一。进行了八年的田间实验,以评估草盖在水和沉积物径流倾斜柑橘土地中的影响。还根据原位土壤水分测量分析土壤湿度制度。在径流剧情实验中进行了四种治疗方法:(1)没有植被,裸陆(BL); (2)常规治疗,没有草覆盖的柑橘(CK); (3)柑橘与百慕大草(sp)的植物; (4)柑橘与百慕大草(FC)的全套封面。结果表明,与CK(311.4mm)和BL(456.7mm)处理相比,使用SP(27.2mm)和Fc(33.0mm)减少了年径流量(P <0.05)。与CK治疗相比,SP和FC处理显着降低了年平均沉积物产量,降低了99.38%至99.67%。在四个深度(0-10,10-20,20-30和30-40cm)的土壤水分变化与季节性降水模式一致。在土壤轮廓内,土壤水分含量随深度增加。在4个深度中的3个中,SP的土壤水分含量(21.20-27.84m(3)/ m(3),平均值)是最高的。由于植物蒸腾量的耗水量低,FC的土壤含水量(14.92-26.30 m(3)/ m(3),平均值)低于SP,但仍然高于CK(16.03-25.00米( 3)/ m(3),平均值)。基于Richards的公式数值模型,优化工具和观察到的土壤水分数据,计算实际蒸散蒸腾,干旱和雨季期间进行了水平衡分析。结果表明,坡地柑橘土地种植草层可以有效地降低地表水径流和土壤侵蚀,增加水浸润,但应注意植物草所引起的干旱风险。与FC相比,干旱期间SP的干旱风险远低得多,SP在雨季期间为根区中的更多水储存。总之,SP是一个建议宜的治疗方法。

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