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Modeling and forecasting groundwater level fluctuations of Shiraz plain using advanced statistical models

机译:使用高级统计模型对设拉子平原的地下水位波动进行建模和预测

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Industrial and agricultural developments cause decreasing groundwater level in the world and Iran also. This tends to drying of water wells, decrease in river flow, lowering of water quality, increase of pumping costs, ground settlements and aquifer death. Shiraz aquifer, area of 270 square kilometer, located in south of Iran. Monthly unit hydrograph data was measured in 16 years 1993 – 2008, calculated with average weighting method. ITSM software is used for all calculations in this research. For achieving a stationary series, trend and seasonal components removed from original data by differencing operator (first with 2 lags and then with 12 lags). Then the autoregressive (order 24) fitted to the series with AIC=165.117. Coefficient of the fitted model finalized by the residual tests. All test of randomness (6 tests) confirmed the selected model. For 5 years in the future, forecast data evaluated by 95% confidence interval. In period of 1993–2008 and 2009–2013, no tremendous reduction in the mean groundwater level recorded or will be seen.
机译:工业和农业的发展导致世界地下水水平下降,伊朗也下降。这往往会导致水井干燥,河流流量减少,水质下降,抽水成本增加,地面沉降和含水层死亡。设拉子含水层,面积270平方公里,位于伊朗南部。 1993年至2008年的16年中使用平均加权法计算了每月的单位水文数据。 ITSM软件可用于本研究中的所有计算。为了获得平稳序列,由差分运算符从原始数据中删除趋势和季节成分(首先有2个滞后,然后有12个滞后)。然后将自回归(24阶)拟合到AIC = 165.117的序列。拟合模型的系数由残差测试确定。所有随机性测试(6个测试)均确认了所选模型。在未来的5年中,预测数据将以95%的置信区间进行评估。在1993年至2008年和2009年至2013年期间,没有记录到或将不会看到平均地下水位的大幅下降。

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