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晋西黄土区不同密度刺槐林对土壤水分的影响

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在晋西黄土区蔡家川流域刺槐林地调查的基础上,选择密度为1 400株/hm2与2 200株/hm2的刺槐林地分别代表研究区低密度和高密度的刺槐林,并以裸地作为对照.通过设立固定样地,定位观测样地0-150 cm土层的土壤水分,研究不同密度刺槐林地土壤水分状况及时空变化规律,并以土壤水分亏缺度和补偿度研究试验区降雨对刺槐林地土壤水分补偿与恢复效应.结果表明:(1)低密度刺槐林年平均土壤储水量比高密度刺槐林年平均土壤储水量绝对值高7.49 mm,且低密度刺槐林达到土壤适宜储水量的天数比高密度刺槐林多60 d;(2)从土壤剖面的垂直方向看,高密度和低密度刺槐林对30 150 cm土层土壤水分消耗量无明显差异,但高密度刺槐林对表层土壤(0-30cm)的消耗远大于低密度刺槐林;(3)综合考虑不同降雨强度下土壤水分恢复程度、降雨补偿土壤深度等指标,研究区高密度刺槐林地土壤水分亏缺相对较大,研究区自然降雨不足以充分补给土壤水分,而低密度刺槐林地土壤水分经降雨补给可恢复到较高的水平.总体来看,研究区低密度刺槐林地土壤水分状况较好,建议研究区刺槐林种植密度以不超过1 400株/hm2为宜.
Influence of Different Densities of Robinia pseudoacacia Forest on Soil Moisture in Loess Region of Western Shanxi Province
On the basis of investigation on Robinia pseudoacacia forestlands in Caijiachuan watershed in loess region of western Shanxi province, R.pseudoacacia forestlands with the densities of 1 400 trees/hm2 and 2 200 trees/hm2 were selected to represent low and high density R.pseudoacacia forests of this region respectively, with the bare land as a control sample plot.Based on the located observation of soil moisture at 0-150 cm soil layer of sample plots, soil moisture condition and its' spatio-temporal changes in forestlands with different densities of R.pseudoacacia were studied, and the effects of rainfall on compensation and rehabilitation of soil moisture in R.pseudoacacia forestlands were investigated by measuring the deficit and compensation degree of soil water storage.The results showed that: (1) The annually average soil water storage of low density R.pseudoacacia forestland was 7.49 mm higher than that of high density R.pseudoacacia forestland, and the period of low density R.pseudoacacia forestland in which soil water storage reached the optimal water storage was 60 days longer than that of high density R.pseudoacacia forestland;(2) in vertical direction of soil profile, there was no significant difference between soil moisture consumption of low and high R.pseudoacacia forestlands at 30-150 cm soil layer, while high density R.pseudoacacia forest consumed more soil water than low density R.pseudoacacia forest at the surface layer of soil (0-30 cm);(3) in consideration of rehabilitation of soil moisture and rainfall compensation depth under different rainfall intensities, it was found out that soil water deficit in high density R.pseudoacacia forestland was relatively greater and natural rainfall wasn't sufficient to compensate the soil moisture;however, soil moisture in low density R.pseudoacacia forestland could recover to high level after raining.On the whole,the soil moisture condition of low density R.pseudoacacia forestland was better.Therefore it is suggested that the planting density of R.pseudoacacia forestland in the study area should be less than 1 400 trees/hm2.

loess region of western Shanxi provinceRobinia pseudoacaciasoil water storagedeficit degree of soil water storagecompensation degree of soil water storage

常译方、毕华兴、许华森、廖文超、蔡智才、王丹

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北京林业大学水土保持学院,北京100083

山西吉县森林生态系统国家野外科学观测研究站,山西吉县042200

晋西黄土区 刺槐 土壤储水量 土壤水分亏缺度 土壤水分补偿度

国家自然科学基金

31470638

2015

水土保持学报
中国土壤学会 中国科学院水利部水土保持研究所

水土保持学报

CSTPCDCSCD北大核心
影响因子:1.226
ISSN:1009-2242
年,卷(期):2015.29(6)
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