基于因子分析的广西平果市土壤地球化学分区及农业种植建议

    Soil geochemical zoning based on factor analysis and recommendations for agricultural planting in Pingguo City, Guangxi

    • 摘要:
      研究目的 本文旨在探讨如何从测试指标多、信息量大的土地质量地球化学调查数据中获取有用的地球化学信息,并为农业种植提供建议。
      研究方法 对广西平果市1∶25 万土地质量地球化学调查表层土壤数据进行因子分析,提取主要因子,根据各样品的因子得分对样品分类,并依据其空间分布特征进行地球化学分区。
      研究结果 研究区表层土壤中有40项指标表现出明显富集,岩溶区有44项指标平均值明显高于非岩溶区;共划分了6个地球化学分区,F1区有37项指标富集,反映了碳酸盐岩成土母岩因子,宜优先发展经济林、果园等对环境扰动少的农业;F2区富集亲生物元素,反映了生物地球化学作用和人类活动因子,宜重点发展蔬菜、热带水果等农业;F3区富集低温成矿元素,反映了构造活动与成矿作用因子,宜因地制宜发展经济林、蔬菜、热带水果等农业;F4区富集Mo和Se,可对富硒土地资源进行进一步评价和开发利用;F5区富集F、MgO,宜优先发展经济林和水源涵养林;F6区有39项指标贫化,反映了碎屑岩成土母岩因子,宜因地制宜发展经济林、蔬菜、热带水果等农业。
      结论 基于因子分析划分的土壤地球化学分区为从宏观上认识土壤元素地球化学分布特征提供了一个“窗口”,同时也为种植区规划、农业种植结构调整、特色农产品开发提供了科学依据。

       

      Abstract:
      This paper is the result of land geochemistry engineering.
      Objective This study aims to explore how to extract useful geochemical information from land quality geochemical survey data, which feature multiple analysis indicators and a large volume of information, and to provide recommendations for agricultural planting.
      Methods Factor analysis was conducted on the topsoil data from the 1∶250 000 land quality geochemical survey in Pingguo City, Guangxi. The main factors were extracted, and the samples were classified based on their factor scores. The geochemical zoning was subsequently carried out according to their spatial distribution characteristics.
      Results In the topsoil of the study area, 40 indicators showed significant enrichment, and the average values of 44 indicators in karst areas were significantly higher than those in non−karst areas. A total of six geochemical zones were delineated. In the F1 area, 37 indicators exhibited enrichment, reflecting the influence of carbonate rock parent materials and it is advisable to prioritize the development of agriculture with minimal environmental disturbance, such as economic forests and orchards. In the F2 area, biophilic elements exhibited enrichment, reflecting biogeochemical processes and anthropogenic factors, and it is recommended to focus on developing agriculture such as vegetables and tropical fruits. In the F3 area, low−temperature ore−forming elements exhibited enrichment, reflecting the influence of tectonic activity and mineralization, and it is suitable to develop agriculture such as economic forests, vegetables, and tropical fruits, taking local conditions into account. In the F4 area, Mo and Se exhibited enrichment, and further evaluation and development of selenium rich land resources can be carried out. In the F5 area, F and MgO exhibited enrichment, and it is advisable to prioritize the development of economic forests and water conservation forests. In the F6 area, 39 indicators exhibited depletion, reflecting the influence of detrital rock parent materials, and it is advisable to develop agriculture such as economic forests, vegetables, and tropical fruits, taking local conditions into account.
      Conclusions Soil geochemical zoning based on factor analysis provides a "window" for understanding the geochemical distribution characteristics of soil elements from a macro perspective. It also offers a scientific basis for planting area planning, adjustment of agricultural planting structures, and development of characteristic agricultural products.

       

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