首页|期刊导航|湖南农业科学|怀化市不同母质发育土壤在中国土壤系统分类的归属

怀化市不同母质发育土壤在中国土壤系统分类的归属OA

Attribution of Soils Developed from Different Parent Materials in Huaihua City in Chinese Soil Taxonomy

中文摘要英文摘要

为了探明湖南省怀化市典型土壤在中国土壤系统分类中的归属,选取怀化市 21 个发育于 7 种母质的土壤剖面样点,分析成土环境、剖面形态特征及土壤理化性质,按中国土壤系统分类方案,检索诊断层和诊断特性,确定其在中国土壤系统分类中的归属.结果表明:该供试土壤的主要诊断层为水耕表层和水耕氧化还原层,土壤剖面氧化还原现象发育显著,呈现典型的水耕人为土剖面发生学特征;21 个土壤剖面归属于富铁土、人为土、淋溶土等 5 个土纲,湿润富铁土、水耕人为土等6 个亚纲,简育湿润富铁土、铁聚水耕人为土等 11 个土类,普通简育湿润富铁土、普通铁聚水耕人为土等 15 个亚类,进一步划分为 17 个土族和 21 个土系.

To clarify the attribution of typical soils in Huaihua City,Hunan Province under the Chinese Soil Taxonomy,this study selected twenty-one soil profile samples developed from seven types of parent materials in Huaihua City to analyze the soil-forming environment,profile morphological characteristics,and soil physicochemical properties based on field observations and laboratory analysis results.According to the Chinese Soil Taxonomy(CST)scheme,diagnostic horizons and characteristics were retrieved to determine the affiliation of soil samples in the CST.The results showed that the tested soil had anthraquic epipedon and hydragric horizon as its main diagnostic horizons.The soil profile exhibited prominent redox features,representing typical profile characteristics of Anthraquic-Anthrosols.Twenty-one soil profiles belonged to five soil orders including Ferrosols,Anthrosols,and Argosols,six suborders including Udic Ferrosols and Stagnic Anthrosols,eleven soil groups including Hapli-Udic Ferrosols and Fe-accumuli-Stagnic Anthrosols,fifteen subcategories including Typic Hapli-Udic Ferrosols and Typic Fe-accumuli-Stagnic Anthrosols,seventeen soil families,and twenty-one soil series.

吴泳晖;夏婷;刘苏;罗恋;欧阳宁相

湖南省怀化市农业综合服务中心,湖南 怀化 418000湖南财政经济学院经济地理学院,湖南 长沙 410205湖南财政经济学院经济地理学院,湖南 长沙 410205湖南财政经济学院经济地理学院,湖南 长沙 410205湖南财政经济学院经济地理学院,湖南 长沙 410205

农业科技

成土母质诊断层诊断特性土壤分类怀化

parent materialdiagnostic horizondiagnostic characteristicssoil taxonomyHuaihua

《湖南农业科学》 2026 (6)

21-31,11

国家自然科学基金青年项目(42501218)湖南省教育厅优秀青年项目(24B0916)

10.16498/j.cnki.hnnykx.2026.006.004

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