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大交盆地地下水位动态分析及预报
ANALYSIS AND FORECAST OF GROUNDWATER REGIME AT DAJIAO BASIN
【摘要】 本文用逐步回归分析法对影响大交盆地地下水位变化的因素进行变量筛选,找出影响地下水位变化的主要因素是近三年的降水量,得出相应的随机数学模型和平稳时间序列线性模型,用其对降水量进行了递推预报,进而对盆地的地下水位进行了预报.认为大交盆地的地下水资源目前不是超采状态.
【Abstract】 Using successive regression analysis method, this paper makes a variable selection for the factors influencing the change of groundwater level of Dajiao basin. The chief factcr is found to be the precipitation of the recent three years. The corresponding stochastic mathematical model and steady time sequence linear model have been found. Using these models, the precipitation is forecasted recursive. Thence, the groundwater level of the basin is forecosted. It is considered that at present the groundwater resource of the Dajiao basin in not over-extracted.
【关键词】 降水量;
地下水位;
逐步回归分析;
平稳时间序列;
递推预报;
【Key words】 precipitation; groundwater table; sucessive regression analysis; steady time sequence; recurrence fcrecasting;
【Key words】 precipitation; groundwater table; sucessive regression analysis; steady time sequence; recurrence fcrecasting;
- 【文献出处】 勘察科学技术 ,Site Investigation Science and Technology , 编辑部邮箱 ,1995年01期
- 【分类号】P641.7
- 【被引频次】2
- 【下载频次】43