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土地利用方式对喀斯特土壤微生物资源限制的影响

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文章选取广西喀斯特地区4种常见土地利用方式(封育、刈割、牧草、玉米种植)为研究对象,分析土壤养分碳(C)、氮(N)、磷(P)相关酶的活性,并基于酶化学计量学方法揭示土壤微生物受何种养分资源限制,以探讨不同土地利用方式对土壤微生物养分资源限制的作用规律.结果表明:不同土地利用方式下土壤的4种酶活性发生显著变化,其与土壤的可利用性养分紧密相关.通过酶化学计量学发现,种植玉米和牧草均显著加剧土壤微生物的C资源限制,这主要由土壤有机碳及微生物生物量碳的减少导致.4种土地利用方式的土壤微生物均受到N的限制,而非P的限制,且刈割和牧草种植会加剧微生物的N限制.相关性分析表明,N资源限制与微生物生物量碳的增加有关,因为微生物同化碳可能需要土壤中更多的可利用氮素.此外,微生物生物量C、N、P与酶化学计量有较强的相关性,很好地解释了不同土地利用方式下微生物资源限制的变化,可作为评估喀斯特土壤微生物资源限制的有效指标.
Effects of land use patterns on the limitation of soil microbial resources in the karst areas of Southwest China
The experimental area is situated in the Mulian comprehensive experimental demonstration zone of Karst Ecosystem Observation and Research Station of Chinese Academy of Sciences,located in Huanjiang Maonan Autonomous County,Guangxi Zhuang Autonomous Region. This region falls within the subtropical monsoon climate zone. The average annual temperature is 19.9℃,with an extreme high of 38.7℃ and an extreme low of-5.2℃. The average annual rainfall is 1,380 mm,characterized by abundant precipitation that is unevenly distributed throughout the seasons;the rainy season accounts for more than 70% of the total annual rainfall. The study area is characterized by a typical karst peak-cluster depression with an elevation of 272.0-647.2 m. The average bedrock exposure in the depression and the sloping land is 15% and 30%,respectively,and their soil depths are 20-160 cm and 10-50 cm,respectively. The soil primarily consists of yellow-brown lime soil and brown lime soil,which have been developed from dolomite. The volume fraction of topsoil gravel can reach 10%-40%. The soil texture is composed of clay loam and clay,with the mass fraction of silt ranging from 25% to 50% and that of clay from 30% to 60%,respectively.Soil microbial growth and activity are often limited by nutrient resources,and understanding which nutrients limit microbial activities is crucial for assessing ecosystem function and developing effective management strategies. Previous studies have shown that soil microorganisms are mainly limited by nutrient carbon © and phosphorus (P) during natural succession after the land has been left uncultivated in karst areas. However,measures such as fertilization in agricultural activities may change microbial resource limitations. In order to investigate nutrient resource limitations of soil microorganisms in agricultural land,this experiment selected four common land use patterns in Huanjiang,Guangxi,including enclosure,mowing,grass planting and corn planting,and analyzed enzyme activities related to C,nitrogen (N) and P in soil. Based on enzyme stoichiometry,the nutrient limitations of soil microorganisms were identified,and the influence of different land use patterns on the changes in microbial resource limitations in soil was clarified. This study could provide valuable guidance for the evaluation and management of different land use ecosystems.The results showed that soil enzyme activities changed significantly under different land use patterns,which was closely related to nutrients available in soil. Through enzyme stoichiometry,it was found that planting maize and grass significantly increased the nutrient C resource limitation of soil microorganisms,which was mainly caused by the reduction of soil organic carbon and microbial biomass carbon. The soil microorganisms of the four land use patterns were limited by N,but not by P. In addition,mowing and grass planting exacerbated the N limitation of microorganisms. Correlation analysis suggested that N resource limitation was associated with an increase in microbial biomass carbon,as microbial assimilation of carbon may require more nitrogen available in soil. In addition,microbial biomass C,N and P were significantly correlated with enzyme stoichiometry,which well explained the changes of microbial resource limitations under different land use patterns,and could be used as an effective index to assess microbial resource limitations in karst soil.In summary,this study indicates that changes in microbial resource limitations in soil should be fully considered in the evaluation and management of different ecosystems in karst areas,which was conducive to formulating more accurate and effective soil management strategies to promote the health and sustainable development of ecosystems. It is suggested to apply organic fertilizer such as manure or straw to alleviate the nutrient C resource limitation of soil microorganisms in karst areas where corn and forage are planted. In karst mowing areas,nitrogen fertilizer needs to be applied moderately to alleviate nutrient N resource limitation of microorganisms and to increase plant productivity.

land usekarst ecosystemmicrobial resource limitationenzyme activityenzyme stoichiometry

肖霜霜、陈武荣、傅伟、张建兵

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南宁师范大学北部湾环境演变与资源利用教育部重点实验室,广西南宁 530001

南宁师范大学广西地表过程与智能模拟重点实验室,广西南宁 530001

中国科学院亚热带农业生态研究所亚热带农业生态过程重点实验室,湖南长沙 410125

中国科学院环江喀斯特生态系统观测研究站,广西环江 547100

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土地利用 喀斯特生态系统 微生物资源限制 酶活性 酶化学计量

2024

中国岩溶
中国地质科学院岩溶地质研究所

中国岩溶

CSTPCD北大核心
影响因子:0.908
ISSN:1001-4810
年,卷(期):2024.43(5)