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作 者:孙淑娟[1] 周勋波[1] 陈雨海[1] 杨国敏[1] 徐德力 杨荣光
机构地区:[1]山东农业大学农学院/作物生物学国家重点实验室,山东泰安271018 [2]泰安市农业气象试验站,山东泰安271000
出 处:《山东农业科学》2008年第7期5-8,共4页Shandong Agricultural Sciences
基 金:国家重点基础研究发展计划项目(2005CB121106);山东省资源节约型社会科技支撑体系建设专项(2006JY06)
摘 要:通过对冬小麦群体分布方式的调节,研究了冬小麦田土壤水分的动态变化。结果表明,不同深度的土壤水变化趋势随土壤层次增深而增加,A与B处理(行株距分别为7 cm×7 cm和14 cm×3.5 cm)在0~90 cm层次与其它处理的差异幅度较大,而100~120 cm土层差异幅度较小。从4种灌溉处理的土壤水分纵深分布比较来看,在不灌溉条件下,A与B处理能够充分利用冬小麦田深层土壤水分,在灌溉条件下,B处理的土壤水分含量高于其它处理,有利于提高浅层土壤的水分含量。The experiment was conducted to study the dynamic changes of soil moisture in wheat field through the regulation of winter wheat population patterns. The results showed that the soil moisture content increased with the soil layer deepening, treatments A and B were obviously distinct from the other treatments at the layer of 0 ~ 90 era, while there were little differences at the 100 ~ 200 cm layer. When compared from ver- tical changes of soil water content, treatments A and B could utilize the soil moisture well in deep layer of wheat field under the condition of no irrigation. Under the irrigated condition, the soil moisture content of treatment B was higher than that of the other treatments, which was propitious to increase the moisture content of superficial soil.
分 类 号:S512.110.1[农业科学—作物学]
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