In order to understand the effect of different interplantation models on the soil and water losses of young tea oil plantations(Camellia oleifera),the soil and water losses of pure tea oil plantation;tea oil + big gre...In order to understand the effect of different interplantation models on the soil and water losses of young tea oil plantations(Camellia oleifera),the soil and water losses of pure tea oil plantation;tea oil + big green bean(Phaseolus aureua);tea oil + peanut(Arachis hypogaea)were investigated for a whole year in Xinyu,located in the central Jiangxi province.The results showed that the surfaced runoff ranged from 102.03～157.29 t·hm-2a-1 with the average of 136.16 t ·hm-2a-1.The less value was observed in the inter-cropped plantation with peanut,and the runoff values from the pure plantation was very similar to that from the inter-cropped plantation with big green bean,and both were greater by 46.21% and 54.17%,respectively,compared with the inter-cropped stand with peanut.The soil erosion was 139.9～341.3 t·km-2a-1 with the average of 239.9 t·km-2a-1,and the values from the inter-cropped plantations with big green bean and peanut increased by 143.96% and 70.40%,respectively,compared with the pure oil stand.The soil erosion in the 3 type stands was all mild.The nutrient loss ranked from great to small value as the following:Ca 4.645 3 kg·hm-2a-1,K 1.402 6 kg·hm-2a-1,Mg 0.265 1 kg·hm-2a-1,P 0.042 6 kg·hm-2a-1,N 0.039 1 kg·hm-2a-1.The loss in the first half year was significantly greater than that in the second half year,regardless inter-cropped or not.The peak value appeared between March and June.The losses of N,P,and K in the inter-cropped plantation with the big green bean were less than those in the inter-cropped stand with peanut.The loss of K in the inter-cropped stand with peanut was almost the same as the pure plantation,however,the losses of N and P in the inter-cropped stand with peanut were less by 50 percent than that in the pure plantation.展开更多
采用室内纯净水人工模拟降雨试验,在坡度为10°、15°、20°、25°坡面,土槽为5 m、10 m两种规格,对两种土壤((土娄)土与黄绵土)分别进行雨强为1.5 mm min-1,的降雨实验,利用三维激光扫描仪对每一场降雨后的坡面进行监...采用室内纯净水人工模拟降雨试验,在坡度为10°、15°、20°、25°坡面,土槽为5 m、10 m两种规格,对两种土壤((土娄)土与黄绵土)分别进行雨强为1.5 mm min-1,的降雨实验,利用三维激光扫描仪对每一场降雨后的坡面进行监测,分析不同坡度对细沟侵蚀的影响,比较两种土壤坡面细沟侵蚀的差异,以及其差异的影响因子。结果表明:(土娄)土土壤颗粒以粉粒与黏粒为主,粉粒占总质量的64.12%,黏粒为28.42%。黄绵土的土壤颗粒以粉粒为主占总质量的67.95%,黏粒与沙粒含量较少,黏粒占14.52%,沙粒占17.53%。在相同条件下,(土娄)土降雨过程中入渗缓慢,产流时间、坡面流速均快于黄绵土,跌坎出现时间也较早,使其更容易产生细沟。(土娄)土的径流量高于黄绵土,在降雨过程中,径流稳定时间较早。(土娄)土侵蚀量高于黄绵土,(土娄)土产沙率呈增加趋势,黄绵土含沙量变化不明显。从坡面细沟发育来看,(土娄)土坡面细沟成平行状分布,黄绵土细沟为较宽树枝状。展开更多
文摘In order to understand the effect of different interplantation models on the soil and water losses of young tea oil plantations(Camellia oleifera),the soil and water losses of pure tea oil plantation;tea oil + big green bean(Phaseolus aureua);tea oil + peanut(Arachis hypogaea)were investigated for a whole year in Xinyu,located in the central Jiangxi province.The results showed that the surfaced runoff ranged from 102.03～157.29 t·hm-2a-1 with the average of 136.16 t ·hm-2a-1.The less value was observed in the inter-cropped plantation with peanut,and the runoff values from the pure plantation was very similar to that from the inter-cropped plantation with big green bean,and both were greater by 46.21% and 54.17%,respectively,compared with the inter-cropped stand with peanut.The soil erosion was 139.9～341.3 t·km-2a-1 with the average of 239.9 t·km-2a-1,and the values from the inter-cropped plantations with big green bean and peanut increased by 143.96% and 70.40%,respectively,compared with the pure oil stand.The soil erosion in the 3 type stands was all mild.The nutrient loss ranked from great to small value as the following:Ca 4.645 3 kg·hm-2a-1,K 1.402 6 kg·hm-2a-1,Mg 0.265 1 kg·hm-2a-1,P 0.042 6 kg·hm-2a-1,N 0.039 1 kg·hm-2a-1.The loss in the first half year was significantly greater than that in the second half year,regardless inter-cropped or not.The peak value appeared between March and June.The losses of N,P,and K in the inter-cropped plantation with the big green bean were less than those in the inter-cropped stand with peanut.The loss of K in the inter-cropped stand with peanut was almost the same as the pure plantation,however,the losses of N and P in the inter-cropped stand with peanut were less by 50 percent than that in the pure plantation.
文摘采用室内纯净水人工模拟降雨试验,在坡度为10°、15°、20°、25°坡面,土槽为5 m、10 m两种规格,对两种土壤((土娄)土与黄绵土)分别进行雨强为1.5 mm min-1,的降雨实验,利用三维激光扫描仪对每一场降雨后的坡面进行监测,分析不同坡度对细沟侵蚀的影响,比较两种土壤坡面细沟侵蚀的差异,以及其差异的影响因子。结果表明:(土娄)土土壤颗粒以粉粒与黏粒为主,粉粒占总质量的64.12%,黏粒为28.42%。黄绵土的土壤颗粒以粉粒为主占总质量的67.95%,黏粒与沙粒含量较少,黏粒占14.52%,沙粒占17.53%。在相同条件下,(土娄)土降雨过程中入渗缓慢,产流时间、坡面流速均快于黄绵土,跌坎出现时间也较早,使其更容易产生细沟。(土娄)土的径流量高于黄绵土,在降雨过程中,径流稳定时间较早。(土娄)土侵蚀量高于黄绵土,(土娄)土产沙率呈增加趋势,黄绵土含沙量变化不明显。从坡面细沟发育来看,(土娄)土坡面细沟成平行状分布,黄绵土细沟为较宽树枝状。
