沧州市土壤墒情变化规律简析
首发时间:2009-03-30
摘要:依据捷地旱情试验站2003-2006年监测资料,深入分析了沧州地区土壤墒情特点,研究了捷地试验站所代表区域(滨海平原区)的土壤墒情变化规律。采用实际观测资料,分析计算土壤消退系数k值,并求出逐月平均k值,建立退墒预报方案。通过绘制降雨量P~雨前土壤含水率θo~雨后增墒△θ相关图,得出增墒计算经验公式,建立了增墒预报方案。两方案经评定,其精度可以满足本地区墒情预报的要求。该墒情预报方案,对合理指导农作物实施灌溉,发展优质、高产、高效农业,合理利用水资源,保持农业生产持续稳定发展,具有重要的意义。
关键词: 墒情预报 土壤消退系数k 降雨量P 雨前土壤含水率θ 雨后增墒△θ
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Cangzhou City Analysis of soil moisture changes
Abstract:Based on the Czechoslovakia drought situation test house 2003-2006 year monitoring data, has analyzed the Cangzhou area soil state of moisture retention characteristic thoroughly, has studied the Czechoslovakia test house represents the region (the Binhai region of no relief) the soil state of moisture retention change rule. Uses the actual observed data, the analysis computation soil retrogression coefficient k value, and extracts month by month average k the value, the establishment draws back the soil moisture forecast plan. After the plan rainfall amount P~ rain soil moisture content θo~ rain increases the soil moisture △θ related chart, obtains increases the soil moisture computation empirical formula, established increased the soil moisture forecast plan. Two plans pass through the evaluation, its precision may satisfy this local state of moisture retention forecast the request. This state of moisture retention forecast plan, to reasonable instruction crops implementation irrigation, development high quality, high production, highly effective agriculture, uses the water resources reasonably, maintains the agricultural production continues the steady progression, has the vital significance.
Keywords: State of moisture retention forecast Soil retrogression coefficient k Rainfall amount P Before the rain, soil moisture content Theta After the rain, increases soil moisture △θ
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