近40年湖南省不同地区耕地土壤肥力变化特征
作者:
作者单位:

(1.湖南省土壤肥料研究所,湖南 长沙 410205;2.中国农业科学院农业资源与农业区划研究所/耕地培育技术国家工程实验室,北京 100081;3.岳阳市农业农村事务中心,湖南 岳阳 414000;4.怀化市农业农村局,湖南 怀化 418000;5.长沙市农业技术推广中心,湖南 长沙 410006;6.湖南永州市农业农村局,湖南 永州 425000)

作者简介:

龙泽东(1992-),博士研究生,助理研究员,主要从事土壤生态研究。E-mail:longzd313@hunaas.cn。

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基金项目:

基金项目:国家重点研发计划课题(2016YFD0300901);区域创新发展联合基金(U19A2048):湖南省农业科技创新资金项目(2023CX73)。


Characteristics and variations of soil fertility in cultivated land across different regions of Hunan Province in the past 40 years
Author:
Affiliation:

(1.Hunan Soil and Fertilizer Institute,Changsha Hunan 410205;2.Institute of Agricultural Resources and Regional Planning,Chinese Academy of Agricultural Sciences/ National Engineering Laboratory for Improving Quality of Arable Land,Beijing 100081;3.Yueyang Agricultural and Rural Affairs Center,Yueyang Hunan 414000;4.Huaihua Agricultural and Rural Bureau,Huaihua Hunan 418000;5.Changsha Agricultural Technology Extension Center,Changsha Hunan 410006;6.Yongzhou Agricultural and Rural Bureau,Yongzhou Hunan 425000)

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    摘要:

    为明确湖南省不同地区耕地土壤肥力演变特征和主控因素,基于湖南省1980年第二次土壤普查和2017年耕地质量监测数据(包括pH、有机质、全氮、有效磷、速效钾),采用模糊数学(Fuzzy)法计算土壤综合肥力指数,通过随机森林模型分析土壤肥力的主控因素。结果表明,1980—2017年湖南省耕地土壤pH呈下降趋势,湘北平原区、湘中湘东丘陵区、湘南丘陵山区、湘西山区pH均值分别下降0.29、0.41、0.19、0.48;湘北平原区、湘南丘陵山区、湘西山区土壤有机质含量基本维持稳定,均值变化幅度在-3.1%~4.4%,湘中湘东丘陵区土壤有机质含量则显著提升,幅度达18.9%;各地区耕地土壤全氮、有效磷和速效钾均呈上升趋势,土壤全氮、土壤速效钾湘中湘东丘陵区提升幅度最大,分别为36.1%和42.6%,土壤有效磷湘南丘陵山区提升幅度最大,为229.8%;2017—2018年湖南省耕地土壤肥力综合指数向0.6~0.8区间集中,全省肥力水平得到提升,随机森林模型分析表明经过近40年演变,不同地区耕地土壤主控因素存在差异,湘北平原区耕地土壤肥力指标的主控因素是有效磷,湘中湘东丘陵区、湘南丘陵山区土壤肥力的主控因素是速效钾,湘西山区是全氮。

    Abstract:

    In order to clarify the evolution characteristics and main controlling factors of cultivated soil fertility in different regions of Hunan Province,based on the second soil census in 1980 and the monitoring data of cultivated land quality in 2017(including pH,organic matter,total nitrogen,available phosphorus and available potassium). The Fuzzy method was used to calculate the soil comprehensive fertility index,and the Random Forest Model was used to analyze the main controlling factors of soil fertility. The results showed that the pH of cultivated soil in Hunan Province showed a downward trend from 1980 to 2017. The average pH values in the northern Hunan(plain area),the central and eastern Hunan(hilly area),the southern Hunan (hilly area)and western Hunan (mountainous area) were decreased by 0.29,0.41,0.19 and 0.48,respectively. The content of soil organic matter in the northern Hunan,the southern Hunan and the western Hunan remained basically stable,with an average range of -3.1%-4.4%. The content of soil organic matter in the central and eastern Hunan increased significantly,with a range of 18.9%. The total nitrogen,available phosphorus and available potassium of cultivated land in all regions showed an upward trend. The maximum increase of soil total nitrogen and soil available potassium in central and eastern Hunan was 36.1% and 42.6%,respectively,and the maximum increase of soil available phosphorus in southern Hunan was 229.8%. From 2018 to 2017,the comprehensive index of cultivated land soil fertility in Hunan Province was concentrated in the range of 0.6-0.8,and the fertility level of the whole province was improved. The random forest model analysis pointed out that after nearly 40 years,the main controlling factors of cultivated land soil in different regions were different. The main controlling factor of cultivated land soil fertility index in the northern Hunan was the available phosphorus. The main controlling factor of soil fertility in the eastern and southern Hunan was available potassium,and total nitrogen in the western Hunan.

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龙泽东,孙耿,黄晶,江帆,冯秋分,吴泳晖,胡明勇,张艳峰,罗尊长,孙梅.近40年湖南省不同地区耕地土壤肥力变化特征[J].中国土壤与肥料,2024,(11):37-48.

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  • 收稿日期:2024-01-14
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  • 录用日期:2024-03-23
  • 在线发布日期: 2025-01-08
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