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Estimating the necessary sampling size of surface soil moisture at different scales using a random combination method

机译:使用随机组合方法估算不同规模的地表土壤水分的必要取样量

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摘要

To develop a sampling strategy of surface soil moisture, a random combination method (RCM) was proposed and used to estimate the necessary sampling size (NSS) of soil moisture at different sampling areas. The RCM was developed based on the bootstrap sampling procedure and consideration of all possible sub-sampling combinations of available data. To examine the method, field experiments were conducted in sampling domains of 10 x 10, 20 x 20, 40 x 40, 55 x 55, 80 x 80, and 160 x 160 m(2). Comparisons of the RCM with other commonly used sampling methods, including the statistical, geostatistical, stratified sampling, and bootstrap methods, indicated that the RCM provided rational and efficient sampling strategies. Under the same accuracy, estimated NSS values using the RCM were much smaller than those by the statistical and bootstrap methods. In addition, the RCM has the advantage of requiring less input information, whereas the statistical and stratified sampling methods require independent data with the normal distribution, the stratified sampling method requires stratified allocation information, and the geostatistical method requires the semivariogram model. The RCM was applied to estimate the NSS of soil moisture at different scales (i.e. squares with sides of 10, 20, 40, 80, and 160 m). Estimated values of the NSS under confidence levels of 90% and 95% with relative errors of 5% and 10% were linearly related to the coefficients of variation calculated from the experimental data. To enhance calculation efficiency of the RCM, the procedure was simplified using a small sub-sample size, which dramatically reduced the computation time for the NSS estimation.
机译:为了制定地表土壤水分的采样策略,提出了一种随机组合方法(RCM),用于估计不同采样区域土壤水分的必要采样量(NSS)。 RCM是根据自举抽样程序并考虑到可用数据的所有可能子抽样组合而开发的。为了检验该方法,在10 x 10、20 x 20、40 x 40、55 x 55、80 x 80和160 x 160 m(2)的采样域中进行了现场实验。将RCM与其他常用采样方法(包括统计,地统计,分层采样和自举方法)进行比较,表明RCM提供了合理而有效的采样策略。在相同的精度下,使用RCM估算的NSS值远小于统计和自举方法的NSS值。另外,RCM具有需要较少输入信息的优点,而统计抽样方法和分层抽样方法需要具有正态分布的独立数据,分层抽样方法需要分层分配信息,而地统计方法则需要半变异函数模型。应用RCM来估算不同尺度(即边长为10、20、40、80和160 m的正方形)的土壤水分的NSS。在90%和95%的置信度下,相对误差为5%和10%时,NSS的估计值与从实验数据计算出的变异系数线性相关。为了提高RCM的计算效率,使用较小的子样本大小简化了该过程,从而大大减少了NSS估计的计算时间。

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