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基于遙感與可拓層次分析的水鹽時(shí)空分異特征研究
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新疆維吾爾自治區(qū)自然科學(xué)基金項(xiàng)目 (2020D01A54)和國家自然科學(xué)基金項(xiàng)目(51369030)


Spatial-temporal Distribution of Water and Salt Based on Remote Sensing and Extension Analytic Hierarchy Process
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    為深入了解干旱綠洲規(guī)?;?jié)水治鹽后區(qū)域尺度水鹽時(shí)空分異特征,,有效控制鹽漬化,以焉耆盆地為研究區(qū),,選取2000,、2005、2015,、2020年長時(shí)序LandSat遙感影像和地表含鹽量,、土壤含鹽量、地表灌水量,、地下水埋深及礦化度等指標(biāo),,借助ENVI和ArcGIS軟件,獲取各指標(biāo)的時(shí)空分布柵格圖件,,將各柵格圖件進(jìn)行標(biāo)準(zhǔn)化處理,,按照可拓層次分析法權(quán)重進(jìn)行空間嵌套并疊加,定量化揭示區(qū)域尺度水鹽時(shí)空分異進(jìn)程,。結(jié)果表明:研究區(qū)鹽漬化經(jīng)歷了2000—2005年擴(kuò)張,、2005—2015年顯著減少、2015—2020年趨于穩(wěn)定3個(gè)階段,,從發(fā)展趨勢看,,研究區(qū)鹽漬化處于減輕并趨于穩(wěn)定態(tài)勢,;鹽漬化嚴(yán)重的區(qū)域主要是博斯騰湖濱;由可拓層次分析法得出各指標(biāo)因子權(quán)重由大到小依次為:地下水埋深(0.325),、地下水礦化度(0.282),、土壤含鹽量(0.198)、地表含鹽量(0.184),、地表灌水量(0.031),,可見,地下水埋深和礦化度是影響區(qū)域水鹽時(shí)空分異的主要驅(qū)動因素,。研究為焉耆盆地控制鹽漬化提供理論依據(jù),,同時(shí)為定量化揭示區(qū)域尺度水鹽時(shí)空分異進(jìn)程提供一種新的方法。

    Abstract:

    The key to effectively control salinization is to deeply understand the spatial-temporal distribution of water and salt at the regional scale after large-scale water-saving and salt control in arid oasis. Yanqi Basin in northwest Xinjiang of China was selected as the research area. LandSat remote sensing and field sampling water and salt data were used to analyze the water and salt migration and accumulation process after large-scale water-saving under changing environment. A total of five indicators, including surface salinity, soil salinity, groundwater salinity, surface irrigation, and groundwater depth were selected in 2000, 2005, 2015 and 2020. The weights of each indicator factor were determined by extension analytic hierarchy process. With the help of ENVI and ArcGIS software, spatial distribution raster maps of each indicator factor were obtained, and each raster map was standardized, the space was nested and superimposed according to the weight of each index factor, so as to get the spatial-temporal distribution of water and salt in the regional scale. The results showed that the salinization in the study area experienced three stages: expansion in 2000—2005, shrinkage in 2005—2015 and stabilization in 2015—2020. The areas with serious salinization were mainly along Bostan Lake, especially Bohu County in the west and Heshuo County in the north of Bostan Lake. Overall, the area of mild saline land was the largest, accounting for 6.17%~11.39%, followed by moderate saline land, accounting for 3.08%~10.65%, the area of heavy saline land was the smallest, accounting for 0.56%~1.10% during 2000—2020; the weight of each factor affecting the spatial-temporal differentiation process of water and salt on a regional scale was ranked as follows: groundwater depth (0.325), groundwater salinity (0.282), soil salinity (0.198), surface salinity (0.184), and surface irrigation (0.031). Groundwater depth and groundwater salinity were the main driving factors affecting the spatial-temporal differentiation of water and salt at regional scales. From the interpreted salinization development trend, the salinization in the study area was alleviated and tended to be stable. 

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王環(huán)波,楊鵬年,劉全明,杜明亮,彭亮.基于遙感與可拓層次分析的水鹽時(shí)空分異特征研究[J].農(nóng)業(yè)機(jī)械學(xué)報(bào),2022,53(6):370-379. WANG Huanbo, YANG Pengnian, LIU Quanming, DU Mingliang, PENG Liang. Spatial-temporal Distribution of Water and Salt Based on Remote Sensing and Extension Analytic Hierarchy Process[J]. Transactions of the Chinese Society for Agricultural Machinery,2022,53(6):370-379.

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  • 收稿日期:2022-03-14
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  • 在線發(fā)布日期: 2022-04-10
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