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澳大利亚北部热带稀树草原的碳平衡。

Carbon balance of a tropical savanna of northern Australia.

作者信息

Chen Xiaoyong, Hutley Lindsay B, Eamus Derek

机构信息

Cooperative Research Centre for the Sustainable Development of Tropical Savannas, Faculty of Science, Information Technology and Education, Northern Territory University, NT 0909, Darwin, Australia.

出版信息

Oecologia. 2003 Nov;137(3):405-16. doi: 10.1007/s00442-003-1358-5. Epub 2003 Aug 26.

Abstract

Through estimations of above- and below-ground standing biomass, annual biomass increment, fine root production and turnover, litterfall, canopy respiration and total soil CO(2) efflux, a carbon balance on seasonal and yearly time-scales is developed for a Eucalypt open-forest savanna in northern Australia. This carbon balance is compared to estimates of carbon fluxes derived from eddy covariance measurements conducted at the same site. The total carbon (C) stock of the savanna was 204+/-53 ton C ha(-1), with approximately 84% below-ground and 16% above-ground. Soil organic carbon content (0-1 m) was 151+/-33 ton C ha(-1), accounting for about 74% of the total carbon content in the ecosystem. Vegetation biomass was 53+/-20 ton C ha(-1), 39% of which was found in the root component and 61% in above-ground components (trees, shrubs, grasses). Annual gross primary production was 20.8 ton C ha(-1), of which 27% occurred in above-ground components and 73% below-ground components. Net primary production was 11 ton C ha(-1) year(-1), of which 8.0 ton C ha(-1) (73%) was contributed by below-ground net primary production and 3.0 ton C ha(-1) (27%) by above-ground net primary production. Annual soil carbon efflux was 14.3 ton C ha(-1) year(-1). Approximately three-quarters of the carbon flux (above-ground, below-ground and total ecosystem) occur during the 5-6 months of the wet season. This savanna site is a carbon sink during the wet season, but becomes a weak source during the dry season. Annual net ecosystem production was 3.8 ton C ha(-1) year(-1).

摘要

通过对地上和地下现存生物量、年生物量增量、细根生产与周转、凋落物、冠层呼吸以及土壤总二氧化碳通量的估算,构建了澳大利亚北部桉树林稀树草原在季节和年度时间尺度上的碳平衡。将此碳平衡与同一地点通过涡度协方差测量得出的碳通量估算值进行比较。该稀树草原的总碳储量为204±53吨碳/公顷,其中约84%在地下,16%在地上。土壤有机碳含量(0 - 1米)为151±33吨碳/公顷,约占生态系统总碳含量的74%。植被生物量为53±20吨碳/公顷,其中39%存在于根系部分,61%存在于地上部分(树木、灌木、草本植物)。年总初级生产力为20.8吨碳/公顷,其中27%发生在地上部分,73%发生在地下部分。净初级生产力为11吨碳/公顷·年,其中8.0吨碳/公顷(73%)由地下净初级生产力贡献,3.0吨碳/公顷(27%)由地上净初级生产力贡献。年土壤碳通量为14.3吨碳/公顷·年。大约四分之三的碳通量(地上、地下和整个生态系统)发生在雨季的5 - 6个月。该稀树草原在雨季是碳汇,但在旱季成为弱碳源。年净生态系统生产力为3.8吨碳/公顷·年。

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