地形对贵州石灰岩分布区土壤属性及土壤类型分布的影响
作者:
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(贵州师范大学地理与环境科学学院,贵州省喀斯特山地生态环境国家重点实验室培育基地,贵州 贵阳 550025)

作者简介:

赵文轩(1996-),硕士研究生,主要从事土壤发生与分类研究。E-mail:i1021649927@163.com。

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基金项目:

基金项目:国家自然科学基金项目(41867001);贵州师范大学学术新苗培养及创新探索专项(黔科合平台人才[2018]5769-23);贵州师范大学博士科研项目(GZNUD[2017]7号)。


The influence of topography on soil properties and type distribution in limestone distribution areas in Guizhou
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(State Key Laboratory Incubation Base for Karst Mountain Ecology Environment of Guizhou Provence,School of Geographic and Environmental Science,Guizhou Normal University,Guiyang Guizhou 550025)

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    摘要:

    为认识贵州喀斯特山区土壤属性分异、土壤类型分布与复杂地形条件的关系。以贵州石灰岩分布区32个典型土壤剖面为研究对象,采集不同地形条件下土壤样品,测定土壤物理化学特性,通过分析各地形因子与土壤属性及土壤类型分异的关系,探讨不同地形条件下土壤的分布特征。结果表明:土壤诊断表层有机碳含量、诊断表下层黏粒阳离子交换量(CEC)和游离氧化铁含量分别在不同海拔范围间差异显著(P<0.05),随着区域海拔的升高,游离氧化铁含量先升高后降低,土壤有机碳含量和黏粒CEC分别在1900 m以下和1400 m以上区域内呈升高态势,富铁土分布与海拔呈负相关关系,多分布于低、中海拔(<1900 m)区域,且随着纬度的升高,分布区域海拔呈降低态势。淋溶土是贵州石灰岩地区分布的主要土壤类型之一(占研究剖面总数的71.87%),随着坡度的增大,土壤pH、盐基饱和度呈升高趋势,分布钙质湿润淋溶土可能性增大。阳坡发育土壤诊断表层厚度显著小于阴坡,阳坡(南、西南)和半阳坡(东南、西)石灰岩山地利于雏形土发育。坡位是显著影响诊断表层有机碳、诊断表下层黏粒CEC和盐基饱和度的地形因子,但对土壤类型分布影响较小。在贵州石灰岩分布区,各地形因子与不同土壤属性存在密切关系,海拔、坡度及坡向对土壤类型分异有一定指示作用。

    Abstract:

    To understand the relationship between soil attribute differentiation,soil type distribution and complex topographical conditions in Guizhou karst mountainous area,32 typical soil profiles in the limestone distribution area of Guizhou were used as the research object,soil samples under different terrain conditions were collected,the physical and chemical properties of the soil were determined,and the distribution characteristics of the soil under the different terrains were discussed by analyzing the relationships among the geomorphological factors,soil attributes and soil types. There were significant differences in soil organic carbon content in the diagnostic surface layer,cation exchange capacity(CEC) and free ferric oxide content of clay in the diagnostic subsurface layer among different altitudes(P<0.05). With the increase of regional altitude,the free ferric oxide content was increased first and then decreased,and the soil organic carbon content and clay CEC showed an increasing trend in the region below 1900 m and above 1400 m,respectively. The distribution of iron-rich soil was negatively correlated with altitude. It was mostly distributed in low and medium altitude (<1900 m)regions,and with the latitude increasing,the altitude of the distribution area showed a downward trend. Leachite is one of the main soil types distributed in limestone areas in Guizhou(accounting for 71.87% of the total number of research profiles). With the increase of slope,soil pH and base saturation showed an increasing trend,and the possibility of calcareous moist leached soil distribution increased. The diagnostic surface thickness of the soil on the sunny slope was significantly smaller than that of the shaded slope,and the limestone mountain areas on the sunny slope(south,southwest)and semi-sun slope(southeast,west)were conducive to the development of embryonic soil. Slope position was a topographical factor that significantly affected the diagnosis of surface organic carbon,the diagnosis of subsurface clay CEC and base saturation,but it had few effects on the distribution of soil types. In the limestone distribution area of Guizhou,there is a close relationship between geomorphic factors and different soil attributes. Altitude,slope,and aspect have different effects on soil types.

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赵文轩,陆晓辉,陈清霞.地形对贵州石灰岩分布区土壤属性及土壤类型分布的影响[J].中国土壤与肥料,2023,(8):1-13.

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  • 收稿日期:2022-07-04
  • 最后修改日期:
  • 录用日期:2022-11-20
  • 在线发布日期: 2023-11-23
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