Researches indicate that dual kriging is a helpful form.
研究表明，克里金法的对偶形是一种有用的形式。
This paper gives a concise introduction to Kriging Method.
本文简要地介绍了克立格法。
The Spatial Variogram plays an important role in Kriging estimation.
空间变异函数在克里格估计中占有重要地位。
We drew a comprehensive environmental quality map by Kriging and GIS.
应用克立格插值法及地理信息系统原理绘制了综合质量图。
Objective: To explore Kriging mapping and its applications in medical map.
目的：探讨“克立格”法及其在医学地图中的应用价值。
The precision of the Ordinary Kriging spherical model was more precise th…
地质统计学方法中，普通克里金球状模型插值精度较高。
Manjiazhai zinc ore body; Kriging Method; ore grade model; calculation of reserves;
曼家寨锌矿体；克里格法；品位模型；储量计算；
Mean soil water content has different spatial distribution according to the Kriging.
克立格插值结果显示不同季节土壤平均含水量的空间分布格局不同。
The result shows that indicator Kriging method can produce better mineral prediction.
结果表明，指示克里格法储量计算能够取得较理想的预测结果。
The paper also deduces factor Kriging equation set while decomposing variation function.
文中在对变差函数进行分解的同时，还推导出因子克里金方程组。
Traditional methods need to fit the Spatial Variogram and then deal with the kriging estimation.
传统的方法需要先进行空间变异函数的拟合，然后进行克里格估计。
Sequential indicator simulation is a kind of stochastic modeling method based on indicator Kriging.
顺序指示模拟方法是以指示克里金为基础的一种随机模拟方法。
Both Yang Chizhong method and Kriging can be used to estimate any variable distributed in space field.
杨赤中法与克立格法，都是对空间域变量进行估计的方法。
In this paper, the Kriging method is used for optimal estimation of the point and areal precipitation.
本文应用克里格法对点雨量和面雨量进行了最优估计。
The overall estimation of slow-release K quality by cokriging was superior to that by ordinary kriging.
缓效钾的协同克立格法的插值精度高于普通克立格法。
Kriging is a basic method in geostatistics. It is often used in geophysical and geochemical data processing.
克立格法是地质统计学的一种基本方法，在非平稳物化探数据处理中经常用到泛克立格方法。
The prediction surface that Ordinary Kriging created and the surface that three-splinecreated are very similar.
同时，普通克立格法与传统航空物探数据内插方法——三次样条函数法所得的表面预测图相似。
Kriging is one of the three dimensional interpolation methods and is now widely used in orebody reserve calculation.
克立格法是三维空间插值的主要方法之一，目前已广泛应用于矿体储量计算过程中。
Based on geostatistics regionalization variable and variogram, kriging interpolation technology was described in detail.
在地质统计学区域化变量、变差函数理论基础上，介绍了克里格插值技术。
Precision of the Kriging interpolation of alkalytic N was improved by 42.8% considering anisotropy of spatial variability.
与各向同性相比，碱解氮在各向异性条件下克里金插值精度提高了42.8%。
Multiple variable indicator Kriging method is also proved to be an alterative for integrated evaluation of soil nutrients.
同时也证明了多变量指标克里格法在土地养分状况的综合评价中应用的可行性。
The fractional geometry model of porosity and permeability was developed based on fractional Kriging interpolation principles.
同时利用分形克里金插值理论，建立了孔隙度和渗透率的分形几何模型。
The algorithm applied the ordinary Kriging method that was originally used in spatial interpolation to construct virtual Wells.
该算法采用原本用于空间插值的普通克里金方法创建虚拟井。
In the process of using Kriging for analysis of Zijin Mine's reserves, the calculation of reserves profile is one of important charts.
在利用克里格方法对紫金矿山进行储量分析的过程中，储量计算剖面图是重要的图件之一。
Kriging maps comparing suggested harvesting had an obvious influence on spatial pattern for soil moisture and temperature in the spring.
克立格空间插值图的比较表明，采伐干扰对土壤表层水分、温度空间格局的影响在春季体现得最为明显。
The geostatistics's basic theories and techniques include the regionalized variables, the semivariance function and Kriging Interpolation.
地统计学的基础理论与方法主要包括：区域化变量、半方差函数、克立格空间插值技术。
The lognormal kriging systems and logarithmic kriging variance are established after non-bias condition and minimum estimation variance are studied.
在分析了无偏条件及最小估计方差之后，给出了对数正态克立格法方程组及对数克立格方差。
Indicator Kriging is a nonparametric statistical method which can make spatial estimation without abandoning peculiar value of reservoir parameters.
指示克立格是一种非参数统计方法，它能在不舍弃特异值的条件下进行有效的空间估计。
The advantages of Kriging method are simple in principle and convenient to computation. It gives a different estimation method from least square collocation.
克立格法具有原理简单、计算方便等优点，它开辟了一条不同于一般最小二乘配置的预测方法。
The ordinary Kriging estimation of rock mass parameters is realized according to these values, and the rock mass parameters in the study field are worked out.
根据理想的实验变差函数参数值，实现岩体参数的普通克立格估计，从而求出研究区域内岩体参数值。
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