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作 者:姜益娟[1] 郑德明[1] 柳维杨[1] 王家强[1] 牛建龙[1]
机构地区:[1]塔里木大学植物科技学院,新疆阿拉尔843300
出 处:《塔里木大学学报》2007年第3期1-5,共5页Journal of Tarim University
基 金:塔里木大学校长基金资助项目(编号:TDZKZD5005)
摘 要:通过对膜下滴灌棉田土壤速效磷钾养分时空分布研究,结果是棉花滴灌水前0-20cm土层水平方向速效磷钾含量变化波动幅度较大,20-60cm土层变化幅度较小。滴水后表层土壤速效磷含量变化波动逐渐变小,速效钾含量变化幅度且较大;0-60cm土层土壤速效磷钾含量自表层垂直向下的分布特点分别是:磷素为10-20cm〉0-10cm〉20-40cm〉40-60cm,钾素为0-10cm〉40-60cm〉10-20cm〉20-40cm;随时间变化特点是:耕层土壤速效磷钾含量从苗期开始均上升,到盛蕾期达最大值,盛蕾期后基本呈直线缓慢递减,不同的是棉花吐絮后土壤速效钾含量回升较快。Though study of space distribution characteristics of soil phosphorus and potassium in under - film trickle irrigation cotton field, it's found that the variety of the content of cotton field soil phosphorus and potassium was : fluctuation was bigger in the horizontal direction in the layers of 0-20cm, while it's smaller in the layersof 20-60cm; phosphorus content fluctuation in the skin soil gradually became small after being trickling and potassium content fluctuation became big; the verdical distribution characteristics of the phos- phorus and potassium from the skin layer to the deep layer in 0-60cm layers respectively were: for phosphorus it's 10 -20cm 〉 0-10cm 〉 20 - 40cm 〉 40 - 60cm; for potassium it's 0 - 10cm 〉 40 - 60cm 〉 10 - 20cm 〉 20 - 40cm ; the characteristics with the time changes were: the content of the phosphorus and potassium in the ploughing layer went up from the seedling stage, and the maximum was reached in the stage of flourishing bud ; then slowly decreased, basically straightly ; what's different was the content of the phosphorus and potassium rised again rapidly after the opening of bolls.
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