首页> 外文期刊>Pedosphere: A Quarterly Journal of Soil Science >Streamflow and Soil Moisture of Agroforestry and Grass Watersheds in Hilly Area
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Streamflow and Soil Moisture of Agroforestry and Grass Watersheds in Hilly Area

机译:丘陵区农林草木小流域径流与土壤水分

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A study was conducted in a hilly area of Sichuan Province, Southwestern China, to compare the streamflow and soil moisture in two upland watersheds with different land use patterns. One was an agroforestry watershed, which consisted mainly of trees with alder (Alnus cremastogyne Burkill) and cypress (Cupressus funebris Endl.) planted in belts or strips with a coverage of about 46%, and the other was a grassland primarily composed of lalang grass (Imperata cylindrica var. major (Nees) C. E. Hubb.), filamentary clematis (Clematis filamentosa Dunn) and common eulaliopsis (Eulaliopsis binata (Retz.) C. E. Hubb) with a coverage of about 44% Streamflow measurement with a hydrograph established at the watershed outlet showed that the average annual streamflow per 100 mm rainfall from 1983 to 1992 was 0 36 and 1.08 L s~(-1) km~(-2) for the agroforestry watershed and the grass watershed, respectively. This showed that the streamflow of the agroforestry watershed was reduced by 67% when compared to that of the grass watershed. The peak average monthly streamflow in the agroforestry watershed was over 5 times lower than that of the grass watershed and lagged by one month. In addition, the peak streamflow during a typical rainfall event of 38.3 mm in August 1986 was 37% lower in the agroforestry watershed than in the grass watershed. Results of the moisture contents of the soil samples from 3 slope locations (upper, middle and lower slopes) indicated that the agroforestry watershed maintained generally higher soil moisture contents than the grass watershed within 0--20 and 20--80 cm soil depths for the upper slope, especially for the period from May through July. For the other (middle and lower) slopes, soil moisture contents within 20-80 cm depth in the agroforestry watershed was generally lower than those in the grass watershed, particularly in September, revealing that water consumption by trees took place mainly below the plow layer. Therefore, agroforestry land use types might offer a complimentary model for tree-annual crop water utilization.
机译:在中国西南四川省的丘陵地区进行了一项研究,比较了两个具有不同土地利用方式的山地小流域的水流和土壤水分。一个是农林分水岭,主要由al木(Alnus cremastogyne Burkill)和柏树(Cupressus funebris Endl。)种植在带状或条状中,覆盖率约为46%,另一种是主要由拉朗草组成的草地(Imperata cylindrica var。major(Nees)CE Hubb。),丝状铁线莲(Clematisfilosa Dunn)和常见的eulaliopsis(Eulaliopsis binata(Retz。)CE Hubb)覆盖了约44%的流量,并在流域建立了水文测量出口表明,农林流域和草地流域从1983年至1992年每100 mm降雨量的年平均流量分别为0 36和1.08 L s〜(-1)km〜(-2)。这表明,与草类流域相比,农林业流域的流量减少了67%。农林分水岭的月平均峰值流量比草木分水岭的峰值平均流量低5倍以上,滞后一个月。此外,在1986年8月典型的38.3 mm降雨事件中,农林流域的峰值流量比草类流域低37%。 3个斜坡位置(上,中,下斜坡)土壤样品的水分含量结果表明,在0--20和20--80 cm的土壤深度内,农林流域的土壤水分含量总体上高于草类流域。上坡,特别是从五月到七月的时期。对于其他(中下部)坡度,农林业流域内20-80厘米深度的土壤水分含量通常低于草木流域,特别是在9月,这表明树木的耗水量主要发生在耕层以下。因此,农林业的土地利用类型可能为树木每年的作物水分利用提供一个补充模型。

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