伊朗马赞达兰平原26年地下水盐度时空变化特征

IF 0.9 4区 地球科学 Q4 GEOCHEMISTRY & GEOPHYSICS Geofizika Pub Date : 2017-06-30 DOI:10.15233/GFZ.2017.34.4
M. Amiri-Bourkhani, M. Khaledian, A. Ashrafzadeh, A. Shahnazari
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引用次数: 6

摘要

地下水资源是伊朗农业部门的主要供水来源之一。因此,本研究旨在调查马赞德兰的地下水盐度状况,以供农业使用。在本研究中,对收集的数据进行了统计分析,选择了适当的半变差函数模型,对预测进行了交叉验证,并使用ArcGIS软件中的地质统计学工具编制了概率图和分区图。为了研究水矿化度的空间变化并绘制水矿化度区划图,使用了普通克里格法(OK)并绘制了水矿化度分区图。电导率(EC)评估的空间结构在大多数年份显示出适度的空间依赖性。EC的分区和概率图显示,地下水的盐度将增加,最可能的盐度与平原东部的低地有关。长期使用这些地下水灌溉会降低水稻产量,并面临严重的水稻生产风险。Mann-Kendall和Sen试验的结果表明,马赞德兰平原EC高于1 dS/m的地下水区域呈下降趋势,这表明平原地下水质量有所改善。
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The temporal and spatial variations in groundwater salinity in Mazandaran Plain, Iran, during a long-term period of 26 years
Groundwater resources are one of the main sources of water supply for agricultural sector in Iran. Therefore, this study aimed to investigate the situation of groundwater salinity in Mazandaran for use in agriculture. In this study, statistical analysis of collected data, proper semivariogram model selection, cross validation of predictions and preparing probabilistic and zoning maps using geostatistical tools in the ArcGIS software, were performed. To investigate the spatial variations and preparing zoning maps of water salinity, ordinary kriging (OK) was used and the zoning maps were prepared. Spatial structure of electrical conductivity (EC) assessment showed a moderate spatial dependence in most years. Zoning and probabilistic maps of EC showed that the salinity of groundwater will be added and the most probable salinity is related the lowland areas in the eastern part of the plain. The use of this groundwater for irrigation in the long term can decrease the rice yield and faced rice production with a serious risk. The results of the Mann-Kendall and the Sen tests indicated a decreasing trend in the area of groundwater with EC higher than one dS/m in Mazandaran plain that this expressing an improvement in the quality of groundwater in the plain.
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来源期刊
Geofizika
Geofizika 地学-地球化学与地球物理
CiteScore
1.60
自引率
0.00%
发文量
17
审稿时长
>12 weeks
期刊介绍: The Geofizika journal succeeds the Papers series (Radovi), which has been published since 1923 at the Geophysical Institute in Zagreb (current the Department of Geophysics, Faculty of Science, University of Zagreb). Geofizika publishes contributions dealing with physics of the atmosphere, the sea and the Earth''s interior.
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