{"title":"Four soil orders on a Vermont mountaintop-one-third of the world`s soil orders in a 2500-square-meter research plot","authors":"T. Villars, S. Bailey, D. Ross","doi":"10.2136/SH15-06-0013","DOIUrl":null,"url":null,"abstract":"As part of the Vermont Long-Term Soil Monitoring Project, five 50 x 50 m plots were established on protected forestland across Vermont. In 2002, ten randomly selected subplots at each monitoring plot were sampled. The 10 pedons sampled at the high-elevation spruce-fir “Forehead” plot on Mount Mansfield were found to include soils of four taxonomic Orders: Entisols, Histosols, Inceptisols, and Spodosols. Soil forming factors such as climate, vegetation, and time are uniform, and podzolization is the major soil forming process, but small variations in parent material thickness and microtopography result in the presence of four orders. A 1-cm difference in the thickness of a horizon can affect the placement of a soil in one of these orders.","PeriodicalId":362488,"journal":{"name":"Soil Horizons","volume":"35 1","pages":"0"},"PeriodicalIF":0.0000,"publicationDate":"2015-11-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"3","resultStr":null,"platform":"Semanticscholar","paperid":null,"PeriodicalName":"Soil Horizons","FirstCategoryId":"1085","ListUrlMain":"https://doi.org/10.2136/SH15-06-0013","RegionNum":0,"RegionCategory":null,"ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"","JCRName":"","Score":null,"Total":0}
引用次数: 3
Abstract
As part of the Vermont Long-Term Soil Monitoring Project, five 50 x 50 m plots were established on protected forestland across Vermont. In 2002, ten randomly selected subplots at each monitoring plot were sampled. The 10 pedons sampled at the high-elevation spruce-fir “Forehead” plot on Mount Mansfield were found to include soils of four taxonomic Orders: Entisols, Histosols, Inceptisols, and Spodosols. Soil forming factors such as climate, vegetation, and time are uniform, and podzolization is the major soil forming process, but small variations in parent material thickness and microtopography result in the presence of four orders. A 1-cm difference in the thickness of a horizon can affect the placement of a soil in one of these orders.
作为佛蒙特州长期土壤监测项目的一部分,在佛蒙特州的保护林地上建立了五个50 x 50米的地块。2002年,在每个监测地块随机抽取10个子地块进行抽样。在曼斯菲尔德山高海拔云杉“前额”样地取样的10个土壤包括4个分类目的土壤:实体土、组织土、初始土和Spodosols。气候、植被、时间等成土因子基本一致,以灰化化为主要成土过程,但母质厚度和微地形的微小变化导致了4级成土的存在。地平面厚度上1厘米的差异就会影响土壤在其中一阶的位置。