首页|以地形为基础的河南省域土壤多样性的格局

以地形为基础的河南省域土壤多样性的格局

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选取河南省作为研究区域,对其DEM数据进行处理得到河南省地形分类图.以地形分类图为基础用经典的土壤构成组分多样性算法计算丰富度指数S、多样性指数H'和均匀度指数E,再使用改进的仙农熵指数(Yh)计算不同地形下每个土类面积占本土类总面积的比例及其在1km×1km网格尺度下的土壤空间分布多样性.结果表明:河南省主要有平原、丘陵、山地和盆地4种地形,且以平原地形为主;河南省有15种土类,从平原、丘陵、山地到盆地地形,土壤丰富度依次递减,且随着地形面积的增加,土类丰富度指数S也不断增加且二者拟合函数为多项式函数;多样性指数H'测度分析显示,4种地形下从土类、亚类到土属多样性值均处于递增趋势,且从平原、丘陵、山地到盆地地形,土类和亚类的多样性值呈”先上升后下降”趋势,土属一直呈“下降”趋势;土属的均匀程度高于土类和亚类的均匀程度,且从平原、丘陵、山地到盆地地形均匀度指数E/土壤构成组分多样性均呈“先上升再下降”趋势;土壤分支率与构成组分多样性间的拟合函数均为多项式函数.经研究,河南省地形和土壤的形成及空间分布多样性有密切的联系,如河南省广阔的平原赋予了潮土分布的地域背景条件,山地地形中山间谷底仅有少量潮土分布,然而平原地形下潮土空间分布斑块多、斑块面积大、空间分布多样性指数高而成为平原地形下空间分布离散性强的优势土壤类型,同时平原也是省内极少面积盐土和碱土仅有的分布区域;同样,山地和丘陵地形下面积最大且空间分布多样性值最大的土类均为褐土;盆地地形以黄褐土、砂姜黑土为主.通过对比,不同地形下指数Yh在空间分布表达上优于其他指数.
Pedodiversity patterns based on Terrain in Henan Province
Henan Province was selected as a case at provincial scale.This study applied the spatial grain size method at 1 km × 1 km grid scale,explored the richness index S,classical soil diversity index H'and the evenness index E.The purpose of this study was to know the classical soil composition diversity in different terrains and the proportion of the area of each soil type in the total area at the same soil group and soil spatial diversity (such as great soil group) using modified Shannon index (Yh).Results showed that there were four different terrain types including plains,hills,mountains and basins based on DEM model in Henan Province.And plain topography was the main terrain.There were 15 soil types (soil group) in Henan Province.And soil richness decreased from plain terrain,hilly terrain,mountain to basin terrain,richness index S increased with the increase of terrain area,and they were fitted with polynomial function.Classical diversity index H'showed increasing trend from soil group,subgroup to soil families.Whereas the diversity value of soil group and subgroup followed "first rise then fall" trend,and that of soil family followed a falling trend.The evenness of soil families was higher than that of soil group and subgroup.And from plain terrain,hilly terrain,mountain to basin terrain,the evenness index E and soil composition component diversity all showed a trend of "first rise and then fall".Soil branch rate and soil composition diversity were fitted with polynomial function.There was close connection among terrain,soil formation and soil spatial distribution diversity in Henan Province.For example,the vast plains provided a good regional background conditions for the distribution of Chao Soil,while narrow area of Chao Soil was distributed at the bottom of mountain valley in mountainous terrain.Chao Soil as the dominant soil type discretely distributed in plain terrain due to large patch number,patch area and diversity index.At the same time,less area of salt and alkali soil was mainly distributed in plain terrain.Cinnamon Soil with the largest area was mostly distributed in mountain terrain and hilly terrain.Huanghe Soil and Shajiang Soil were the major soil types in basin terrain.By contrast,spatial distribution index Yh was better than the other indices in the expression of soil spatial distribution under different terrains.

Henan ProvinceDEMTerrainPedodiversity

任圆圆、张学雷

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郑州大学水利与环境学院,河南郑州450001

自然资源与生态环境研究所,河南郑州450001

河南省 DEM 地形 土壤多样性

国家自然科学基金

41571208

2017

土壤通报
中国土壤学会

土壤通报

CSTPCD北大核心
影响因子:0.818
ISSN:0564-3945
年,卷(期):2017.48(1)
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