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[不同土壤类型对贵州中部喀斯特石漠化地区常见乡土植物叶片δ13C值的影响]

[Effects of different soil types on the foliar δ13C values of common local plant species in karst rocky desertification area in central Guizhou Province].

作者信息

Du Xue-lian, Wang Shi-jie, Luo Xu-qiang

出版信息

Huan Jing Ke Xue. 2014 Sep;35(9):3587-94.

Abstract

By measuring the foliar δ13C values of common local plant species grown in different soil types in Wangjiazhai catchments, a typical karst desertification area in Qingzhen City, Central Guizhou, we studied the impact of soil type and rocky desertification grade on the foliar δ13C values. The results showed that the foliar δ13C values were more negative in yellow soil area than those in black calcareous area and there was no obvious difference in foliar δ13C values between these two soil types. The distribution interval of foliar δ13C values in yellow soil area was narrower than those in black calcareous area and the variation coefficient of foliar δ13C values in yellow soil area were smaller than those in black calcareous area. With increasing degree of karst rocky desertification, the foliar δ13C values of plant community in black calcareous area increased, whereas those in yellow soil area first increased and then decreased. The result of multiple comparison showed that the difference in foliar δ13C values of plant community among rocky desertification grade was not obvious in yellow soil area, but it was obvious in black calcareous area. Correlation analysis between the foliar δ13C values of plant species and the main environmental factors indicated that slope and soil thickness were the main factors which affected the foliar δ13C values of plants in yellow soil area and soil water contant was the main factor in black calcareous area. The impact of soil on the foliar δ13C values was realized by adjusting the soil moisture in study area.

摘要

通过测定贵州中部清镇市典型喀斯特石漠化地区王家寨小流域不同土壤类型上生长的常见本地植物物种的叶片δ13C值,我们研究了土壤类型和石漠化等级对叶片δ13C值的影响。结果表明,黄壤区叶片δ13C值比黑色石灰土区更负,且这两种土壤类型的叶片δ13C值无明显差异。黄壤区叶片δ13C值的分布区间比黑色石灰土区窄,黄壤区叶片δ13C值的变异系数比黑色石灰土区小。随着喀斯特石漠化程度的增加,黑色石灰土区植物群落的叶片δ13C值增加,而黄壤区则先增加后降低。多重比较结果表明,黄壤区植物群落叶片δ13C值在石漠化等级间差异不明显,而黑色石灰土区差异明显。植物物种叶片δ13C值与主要环境因子的相关分析表明,坡度和土壤厚度是影响黄壤区植物叶片δ13C值的主要因素,而土壤含水量是黑色石灰土区的主要因素。在研究区,土壤对叶片δ13C值的影响是通过调节土壤水分来实现的。

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