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首页> 外文期刊>African Journal of Biotechnology >Soil water distribution on different number of growing years of alfalfa pasture in the Loess Plateau of Northwest China
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Soil water distribution on different number of growing years of alfalfa pasture in the Loess Plateau of Northwest China

机译:黄土高原苜蓿草不同生长年限的土壤水分分布

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The alfalfa pastureland in the semiarid Loess Plateau region of Northwest China usually has dry soil layers. We studied the soil water variations on alfalfa (Medicago sativa?L.) grassland with different number of growing years. Seven growing years of alfalfa grassland were chosen in this study: (1) 4-year-old, (2) 6-year-old, (3) 8-year-old, (4) 12-year-old, (5) 14-year-old, (6)18-year-old and (7) 26-year-old. The results showed that the highest soil water content, 12.0 -17.15%, with different number of growing years of alfalfa grassland occurred in 80 -100 cm soil layer, but gradually became stable below 300 cm soil layer. The soil water content with 4, 6 and 8 year alfalfa grassland was in the range of 13.66 - 14.76%, with 12 and 14 year ranged within 11.76 -1 1.87% and with 18 and 26 year within 10.5%. We also found that in 0 - 1000 cm soil layer, the soil water content with different number of growing years of alfalfa grassland had differences due to different soil water conditions and water-supplying capability. The soil water content with 4 and 6 year were 13.85 and 14.22%, respectively, with 8, 12 and 14 year were 12.98, 11.25 and 11.22%, respectively, and with 18 and 26 year were 10.27 and 10.76%, respectively. After alfalfa grew for >18 years, the annual recovery of its soil water at 0 - 200 cm soil depth was 1.49%, whereas the soil water with 18 and 26 year alfalfa pastureland at 200 - 1000 cm soil depth was only 10.10%, dry soil layers occurring in alfalfa pasture. The dry soil layer of alfalfa grassland appears at 160 - 600 cm soil depth in the Loess Plateau. We found that at 250 - 350 cm soil depth, the soil water content with 4 and 6 year alfalfa grassland was in the range of 10.23 - 10.48%, presenting slightly dry soil layer and for more than 8 year, alfalfa was in the range of 7.78 - 8.48%, presenting moderately dry soil layer. In summary, the soil water use of alfalfa would grow with the number of growing years and the depth of desiccated layers will become intensified and thicker.
机译:中国西北半干旱黄土高原地区的苜蓿牧场通常具有干燥的土壤层。我们研究了不同生长年限的紫花苜蓿(Medicago sativa?L。)草地上土壤水分的变化。本研究选择了七个苜蓿草生长年限:(1)4岁,(2)6岁,(3)8岁,(4)12岁,(5 )14岁,(6)18岁和(7)26岁。结果表明,不同苜蓿草生长年限的最高土壤含水率为12.0 -17.15%,发生在80 -100 cm土层,而在300 cm土层以下逐渐稳定。 4、6和8年苜蓿草地的土壤水分含量在13.66-14.76%的范围内,其中12和14年介于11.76 -1 1.87%的范围内,而18和26年介于10.5%的范围内。我们还发现,在0-1000 cm的土壤层中,由于不同的土壤水分条件和供水能力,苜蓿草的不同生长年限的土壤含水量存在差异。 4年和6年的土壤含水量分别为13.85和14.22%,8、12和14年的土壤含水量分别为12.98、11.25和11.22%,18和26年的土壤含水量分别为10.27和10.76%。苜蓿生长超过18年后,在0-200厘米土壤深度下其土壤水的年回收率为1.49%,而在18-26年苜蓿牧场在200-1000厘米土壤深度下的土壤水的年回收率仅为10.10%,干燥苜蓿草中的土壤层。黄土高原苜蓿草原的干燥土壤层出现在土壤深度为160-600 cm处。我们发现在250-350 cm的土壤深度下,4年和6年紫花苜蓿草地的土壤含水量在10.23-10.48%的范围内,呈现出稍微干燥的土壤层,而8年以上,苜蓿的土壤含水量在10-23 cm的范围内。 7.78-8.48%,土壤土层适中。总之,紫花苜蓿的土壤用水量将随着生长年限的增加而增加,并且干燥层的深度将变得越来越深。

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