尼日利亚西南部Ayepe-Olode水源水质及插值程序对选定参数可视化的影响

IF 0.3 Q4 REMOTE SENSING
A. Eludoyin, O. S. Ijisesan
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引用次数: 1

摘要

数据插值——在一组离散的已知数据点范围内构建新的数据点——是地理研究中的一项重要建模活动。在这项研究中,研究了三种常用的插值方法(最近点法、克里格法和移动平均法),以评估尼日利亚Ife South地方政府区一个不断发展的商业中心棕榈油加工区流载废水的选定物理和化学参数的变化分散性。具体目标是检查接收棕榈油流出物的溪流的选定理化性质,并将使用推导的变差函数值的克里格插值结果与基于流行地理信息系统中可接受的参数默认值的结果进行比较。该研究还展示了基于普通克里格、移动平均和最近点插值的选定参数插值的可视化结果。利用PAST3和ILWIS GIS软件进行了分析。结果表明,尽管该河流容易受到该地区周围棕榈油加工活动的污染,但它也会受到本研究未调查的其他非来源点的污染。研究还表明,不同的点插值方法并没有产生相似的结果。尽管使用克里格插值将电导率值插值为120.1–219.5μScm-1,但使用最近点插值和移动平均插值,电导率值分别为105.6–220.0μScm-1和135.0–173.9μScm-1。此外,尽管计算的变差函数模型产生了高斯模型的最佳拟合线,但球形模型被假设为选定GIS软件中所有分布的默认值,因此当Nugget的值实际随数据位置分布而变化时,它被假设为0.00。总之,估计空间变化的过程总是产生受数据分布和模型假设影响的结果,因此,在地理空间评估中,数据特征而不是GIS软件的默认值是合适的。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Water quality and influence of interpolation procedure on visualization of selected parameters in a headwater stream, in Ayepe-Olode, southwestern Nigeria
Data interpolation – construction of new data points within range of a discrete set of known data point – is an important modeling activity in geographical studies. In this study, three commonly applied interpolation methods (nearest point, kriging and moving average) were examined in an assessment of the varying dispersion of selected physical and chemical parameters of stream-borne effluents from palm oil processing area in a growing commercial centre in Ife South local government area in Nigeria. Specific objectives were to examine selected physiochemical properties of a stream that receives palm oil effluent, and compare results of a kriging interpolation using derived variogram values with that which was based on the accepted parametric default in a popular geographical information system. The study also presents visualised results of interpolation of selected parameters based on ordinary kriging, moving average and nearest point interpolation. Analysis were achieved using PAST 3 and ILWIS GIS software. Result showed that although the stream is vulnerable to contamination by the palm oil processing activities around the area, it also receives contaminants from other non-source points that were not investigated in this study. It also indicated that the different point interpolation methods did not produce similar results. Whereas the values of conductivity were interpolated to vary as 120.1 – 219.5 μScm-1 with kriging interpolation, it varied as 105.6 – 220.0 μScm-1 and 135.0 – 173.9 μScm-1, with nearest point and moving average interpolations, respectively. Also, whereas the computed variogram model produced the best fit lines with Gaussian model, the Spherical model was assumed default for all the distributions in selected GIS software, such that the value of Nugget was assumed as 0.00, when it actually varies with data locations distribution. Conclusively, procedure of estimating spatial variation always produce results that are influenced by data distribution and model assumptions, and as such the data characteristics rather than GIS software’s defaults are appropriate for consideration in geospatial evaluation.
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