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[降水变化对中国荒漠草原植物群落多样性及土壤C:N:P生态化学计量特征的影响]

[Effects of Precipitation Changes on Plant Community Diversity and Soil C:N:P Ecological Stoichiometric Characteristics in a Desert Steppe of China].

作者信息

Gao Jiang-Ping, Zhao Rui-Feng, Zhang Li-Hua, Wang Jun-Feng, Xie Zhong-Kui

机构信息

College of Geography and Environment Science, Northwest Normal University, Lanzhou 730070, China.

Gaolan Comprehensive Experimental Station of Ecology and Agriculture, Northwest Institute of Ecology and Environment and Resources, Chinese Academy of Sciences, Lanzhou 730000, China.

出版信息

Huan Jing Ke Xue. 2021 Feb 8;42(2):977-987. doi: 10.13227/j.hjkx.202007041.

Abstract

Studying the influence of precipitation patterns on plant community diversity, soil C:N:P ecological stoichiometric characteristics, and the relationships between key soil factors and plant community diversity is of great significance for the protection of plant community diversity in desert grasslands. This paper was studied in the desert steppe of the west of Loess Plateau using a three-year precipitation manipulation experiment (40% reduction in precipitation, 20% reduction in precipitation, natural precipitation, 20% increase in precipitation, and 40% increase in precipitation), explored the influence of changes in precipitation in dry and wet years on the diversity of plant community and soil C:N:P ecological stoichiometric characteristics. And we also explored the relationship between soil C:N:P ecological stoichiometric characteristics and the key soil factors and the diversity of plant community under changes in precipitation. The results showed that in a normal year and the drier year (2013 and 2015), Patrick richness and Shannon-Wiener diversity index were significantly low under the 20% reduction treatment compared with the control and 40% increase treatments, respectively. During the wetter year, Patrick richness and Shannon-Wiener diversity index were no different between any of the precipitation treatments. In the normal year and the drier year, the soil organic carbon (SOC), total nitrogen (TN), and total phosphorus (TP) contents and the carbon-nitrogen ratio (C:N), carbon-phosphorus ratio (C:P), and nitrogen-phosphorus ratio (N:P) all decreased with an increase in precipitation (the decrease in the C:N ratio was statistically significant). During the wetter year, SOC, TN, C:P, and N:P increased with an increase in precipitation. During the normal year, precipitation treatments had no significant influence on soil water content, having a limited influence on the plant community. TN, N:P, SOC, C:N, and microbial biomass nitrogen (MBN) had a more prominent influence on plant community diversity. In the wetter year, precipitation was abundant leading to a rise in soil nutrients. Water was not the most important factor limiting to plant growth whereas soil water content, soil nutrients, and ecological stoichiometric characteristics jointly regulate plant community diversity. In the drier years, precipitation treatments had a significant impact on soil water content, whereby an increase in precipitation led to high losses of soil nutrients. Therefore, soil water content was the most important factor affecting plant community diversity during drier years. These observations indicate that under dry and wet years, plant community diversity and soil C:N:P ecological stoichiometric characteristics have variable responses to precipitation and soil C:N:P effect on plant community were also different. These results provide a theoretical basis for the protection and management of desert steppe systems under future projected changes in precipitation.

摘要

研究降水格局对植物群落多样性、土壤碳氮磷生态化学计量特征的影响,以及关键土壤因子与植物群落多样性之间的关系,对于保护荒漠草原植物群落多样性具有重要意义。本文在黄土高原西部的荒漠草原开展了为期三年的降水控制实验(降水减少40%、降水减少20%、自然降水、降水增加20%、降水增加40%),探究干湿年份降水变化对植物群落多样性和土壤碳氮磷生态化学计量特征的影响。同时,我们还探究了降水变化下土壤碳氮磷生态化学计量特征与关键土壤因子及植物群落多样性之间的关系。结果表明,在正常年份和较干旱年份(2013年和2015年),与对照和降水增加40%处理相比,降水减少20%处理下的Patrick丰富度和Shannon-Wiener多样性指数分别显著较低。在较湿润年份,各降水处理间的Patrick丰富度和Shannon-Wiener多样性指数无差异。在正常年份和较干旱年份,土壤有机碳(SOC)、全氮(TN)、全磷(TP)含量以及碳氮比(C:N)、碳磷比(C:P)和氮磷比(N:P)均随降水增加而降低(碳氮比降低具有统计学意义)。在较湿润年份,SOC、TN、C:P和N:P随降水增加而增加。在正常年份,降水处理对土壤含水量无显著影响,对植物群落的影响有限。TN、N:P、SOC、C:N和微生物生物量氮(MBN)对植物群落多样性的影响更为突出。在较湿润年份,降水充足导致土壤养分增加。水分不是限制植物生长的最重要因素,而土壤含水量、土壤养分和生态化学计量特征共同调节植物群落多样性。在较干旱年份,降水处理对土壤含水量有显著影响,降水增加导致土壤养分大量流失。因此,在较干旱年份,土壤含水量是影响植物群落多样性的最重要因素。这些观察结果表明,在干湿年份,植物群落多样性和土壤碳氮磷生态化学计量特征对降水的响应不同,且土壤碳氮磷对植物群落的影响也不同。这些结果为未来预计降水变化下荒漠草原系统的保护和管理提供了理论依据。

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