[1]郑雄伟,张响荣,王瑞杰,等.洪湖市土壤酸碱度趋势分析及影响因素[J].华东地质,2023,44(02):197-205.[doi:10.16788/j.hddz.32-1865/P.2023.02.008]
　ZHENG Xiongwei,ZHANG Xiangrong,WANG Ruijie,et al.Trend analysis and influencing factors of soil pH in Honghu City, Hubei Province[J].East China Geology,2023,44(02):197-205.[doi:10.16788/j.hddz.32-1865/P.2023.02.008]
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洪湖市土壤酸碱度趋势分析及影响因素()
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《华东地质》[ISSN:2096-1871/CN:32-1865/P]

卷:
44
期数:
2023年02期
页码:
197-205
栏目:
土壤资源专题
出版日期:
2023-06-17

文章信息/Info

Title:
Trend analysis and influencing factors of soil pH in Honghu City, Hubei Province
作者:
郑雄伟1;  张响荣2;  王瑞杰1;  王晓龙3;  孙为国1
1. 湖北省地质局地球物理勘探大队, 湖北 武汉 430056;
2. 湖北省地质实验测试中心, 湖北 武汉 430034;
3. 中国科学院南京地理与湖泊研究所, 江苏 南京 210008
Author(s):
ZHENG Xiongwei1;  ZHANG Xiangrong2;  WANG Ruijie1;  WANG Xiaolong3;  SUN Weiguo1
1. Geophysical Exploration Brigade of Hubei Geological Bureau, Wuhan 430056, Hubei, China;
2. Hubei Geological Experiment and Test Center, Wuhan 430034, Hubei, China;
3. Nanjing Institute of Geography and Limnology Chinese Academy of Sciences, Nanjing 210008, Jiangsu, China
关键词:
土壤酸碱度; 土壤类型; 成土母质; 湖北省洪湖市
Keywords:
soil acidity and alkalinity; soil type; parent soil; Honghu City;  Hubei Province
分类号:
S153.4
DOI:
10.16788/j.hddz.32-1865/P.2023.02.008
摘要:
洪湖市土地质量地球化学评价工作获得了大量地球化学数据,对近4年所取得的数据进行整体研究,系统分析了所属各乡镇农用地土壤酸碱度。结果表明:该市土壤酸碱度总体特征表现为南部、北部乡镇的土壤酸碱度大于中部乡镇;土壤pH值从西向东逐渐升高,从北向南变化不明显;不同类型土壤对土壤酸碱度的影响由大到小依次为: 沙土型潮土>沙土型灰潮土>浅色草甸土=壤土型灰潮土>灰潮土田>黏土型灰潮土>浅灰潮土田>灰青泥田>壤土型潮土>烂泥田>青泥田>黏土型潮土>浅潮土田>黄棕壤;不同成土母质的pH值由大到小依次为:河流冲积物>湖泊沉积物>第四系黏土沉积物>河流沉积物>红砂岩风化物。洪湖市土壤平均pH值在1982—2007年降低了0.87个单位,在2007—2014年升高了0.35个单位,在2014—2019年又升高了0.47个单位。该研究成果可为地方政府开展耕地质量保护、耕地酸化治理、农业产业结构调整等提供决策参考。
Abstract:
A large amount of geochemistry data has been obtained through the Land Quality Geochemistry Assessment Project in Honghu City, Hubei Province. Based on the overall study on the project data acquired over the past four years, the soil acidity and alkalinity of agricultural land in each town is analyzed systematically. The results show that the soil acidity and alkalinity in the southern and northern towns are higher than those in the middle towns. The trend analysis shows that the soil pH values increases gradually from west to east but does not change obviously from north to south. The influence on soil pH values from different types of soil is descending in following order: sandy soil type fluvo-aquic soil> sandy soil type calcareous fluvo-aquic soil> light-colored meadow soil=loamy calcareous fluvo-aquic soil> calcareous soil field> clay calcareous fluvo-aquic soil> shallow calcareous fluvo-aquic soil> calcareous cyan muddy field> loamy fluvo-aquic soil> muddy field> cyan muddy field> clay fluvo-aquic soil> shallow fluvo-aquic soil filed> yellow brown soil. In addition, the pH values of different parent materials are in descending order as follows:alluvial sediments> lake sediments> Quaternary clay sediments> river sediments> red sandstone weathering materials. The average pH value of soil in Honghu decreases by 0.87 units from 1982 to 2007, increases by 0.35 units from 2007 to 2014, and increases by 0.47 units from 2014 to 2019. The research results can provide decision-making reference for the local government to protect the quality of cultivated land, control the acidification of cultivated land and adjust the structure of agricultural industry.

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备注/Memo

备注/Memo:
收稿日期:2021-7-23;改回日期:2022-11-22。
基金项目:湖北省财政资金项目"湖北省"金土地"工程-高标准基本农田地球化学调查 (编号:HBJTD 20140107、HBJTD20160110、 HBJTD 20170106)"与"洪湖市全域土地质量地球化学评价暨地方特色农业硒资源调查(编号:洪土资函12号)"等项目联合资助。
作者简介:郑雄伟,1986年生,男,高级工程师,博士生,主要从事生态环境地球化学调查工作。Email:493928635@qq.com。
通讯作者:张响荣,1984年生,女,工程师,硕士,主要从事样品分析测试工作。Email:301012239@qq.com。
更新日期/Last Update: 1900-01-01