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高寒草甸土壤团聚体碳氮磷对退化的响应及其影响因素 被引量:3
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作者 孙建波 李成阳 +4 位作者 赖炽敏 陈洋 陈小杰 周俊 彭飞 《草地学报》 CAS CSCD 北大核心 2023年第4期1106-1114,共9页
植物和土壤微生物是土壤团聚体黏合物和养分的重要来源,因此土壤团聚体组成及其养分库的变化可指示生态系统退化过程。本文在长江源区根据植被群落特征选取未退化、中度和严重退化高寒草甸,研究其土壤中大团聚体(>250μm)、微团聚体(... 植物和土壤微生物是土壤团聚体黏合物和养分的重要来源,因此土壤团聚体组成及其养分库的变化可指示生态系统退化过程。本文在长江源区根据植被群落特征选取未退化、中度和严重退化高寒草甸,研究其土壤中大团聚体(>250μm)、微团聚体(55~250μm)和游离态粉粒黏粒(<55μm)含量、不同粒级团聚体碳氮磷含量及储量随草地退化的变化特征,并分析了植物和微生物活动与这些变化特征的关系。结果表明:未退化和中度退化高寒草甸土壤以微团聚体为主。退化使高寒草甸大团聚体和微团聚体碳氮含量及储量显著下降,但磷含量及储量未发生显著变化。游离态粉粒黏粒氮磷储量在严重退化高寒草甸显著增加。各团聚体碳氮含量与地上生物量和微生物量碳正相关,磷含量与微生物量碳负相关。本研究表明植物及受其影响的土壤微生物变化是造成高寒草甸退化后不同团聚体碳氮磷库变化的主要原因。 展开更多
关键词 草地退化 团聚体 碳氮磷含量 高寒草甸 青藏高原
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Degradation stage effects on vegetation and soil properties interactions in alpine steppe 被引量:2
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作者 LI Cheng-yang PENG Fei +6 位作者 XUE Xian lai chi-min ZHANG Wen-juan YOU Quan-gang CHEN Xiao-jie ZHANG Xue-qin WANG Tao 《Journal of Mountain Science》 SCIE CSCD 2021年第3期646-657,共12页
In recent decades,overgrazing and the warming and drying climate have resulted in significant degradation of alpine grasslands in the source region of the Yellow River.However,research into the relationships between v... In recent decades,overgrazing and the warming and drying climate have resulted in significant degradation of alpine grasslands in the source region of the Yellow River.However,research into the relationships between vegetation and soil properties has mainly focused on an overall degradation stage,and few studies have investigated which soil properties can impact vegetation change at different stages of degradation.Vegetation and soil properties were observed in the field and measured in the laboratory for different predefined stages of degradation for alpine grassland in Maduo County in the source region of the Yellow River.Results show that:1)the aboveground and belowground biomass,soil organic carbon,total nitrogen,nitrate,and ammonia content did not decrease significantly from the intact to moderate degradation stage,but decreased significantly at severe and very severe stages of degradation;2)dominant plant species shifted from gramineaes and sedges to forbs;3)the species richness and Pielou evenness indices decreased significantly at the very severe degradation stage,the Shannon-Wiener diversity index increased at the slight and moderate degradation,but decreased at the severe and very severe degradation stages;4)soil bulk density was the strongest soil driver for changes in the plant biomass and community diversity at the intact,slight and moderate degradation stages,whereas soil organic carbon and nitrate nitrogen content were the main driving factors for changes in plant biomass and diversity at the severe and very severe degradation stages.Our results suggest that there may be different interactions between soil properties and plants before and after moderate stages of degradation. 展开更多
关键词 Land degradation BIOMASS Soil nutrient Species diversity Qinghai-Tibetan Plateau
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