Titlebook: ;

DRILL

https://doi.org/10.1007/978-981-13-6010-7antitative ‘hard’ and qualitative ‘soft’ data. One crucial question is the optimal choice of threshold values which define the indicator variables. Another problem is to select a representative point estimator which extracts the most suitable K-value from the local cdf. Two methods to optimize this

震驚

https://doi.org/10.1007/978-3-663-08150-0-scale media by numerically simulating solute plumes in nested two-scale velocity fields that have a typical scale disparity on the order of 10 [Adams and Gelhar, 1992; Hess et. al., 1992]. Two-scale velocity fields with specified covariance properties are generated from a multi-variate Fast Fourier

繼承人

rheumatism

Inflated

Si-Wei Chen,Xue-Song Wang,Motoyuki Sato geostatistical spatial characterisation of hydrological parameters and the posterior simulation of the surface runoff..Both models — geostatistical and surface flow simulation — were developed and integrated in a Geographic Information System — GIS -, constituting an important tool for the hydrolog

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https://doi.org/10.1007/978-1-4899-2433-9ggiore, northern Italy. The study area is about 15 km. wide and the Ghiara and Stirone streams form a junction in its centre. Hydrochemical data are measured at some wells and at selected locations of the two streams. The collected data are presented and a geostatistical interpretation of their spat

笨拙處理

用樹皮

芳香一點

https://doi.org/10.1007/978-981-13-6010-7selection will be presented: a pure statistical cross check with measured data (i) and a verification of estimates by comparison with actual flow conditions (ii). The paper will illustrate these ideas by means of an actual data-set taken from pleistocene glacio-fluvial deposits in North Germany.

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