東華大學圖書館 |

語系: 繁體中文

說明(常見問題)

回圖書館首頁

手機版館藏查詢

登入

回首頁

切換: 標籤 | MARC模式 | ISBD

Biogeochemical cycling and microbial...

Attaeian, Behnaz.

FindBook

Google Book

Amazon

博客來

Biogeochemical cycling and microbial communities in native grasslands: Responses to climate change and defoliation.

紀錄類型:	書目-語言資料,印刷品 : Monograph/item
正題名/作者:	Biogeochemical cycling and microbial communities in native grasslands: Responses to climate change and defoliation./
作者:	Attaeian, Behnaz.
面頁冊數:	217 p.
附註:	Source: Dissertation Abstracts International, Volume: 71-05, Section: B, page: 2903.
Contained By:	Dissertation Abstracts International71-05B.
標題:	Climate Change. -
電子資源:	http://pqdd.sinica.edu.tw/twdaoapp/servlet/advanced?query=NR60510
ISBN:	9780494605103

Biogeochemical cycling and microbial communities in native grasslands: Responses to climate change and defoliation.
Attaeian, Behnaz.

Biogeochemical cycling and microbial communities in native grasslands: Responses to climate change and defoliation. - 217 p.

Source: Dissertation Abstracts International, Volume: 71-05, Section: B, page: 2903.

Thesis (Ph.D.)--University of Alberta (Canada), 2010.

Ongoing climate change has emerged as a major scientific challenge in the current century. Grassland ecosystems are considered net carbon (C) sinks to mitigate climate change. However, they are in turn, influenced by climate change and management practices, providing feedback to climate change via soil microbial community and biogeochemical fluxes. In this thesis, I examined the impact of warming, altered precipitation, and defoliation on soil microbial composition and function, C and N dynamics, and fluxes in soil respiration (CO2), nitrous oxide (N2O) and methane (CH 4), together with other belowground ecosystem functions, within two ecosites in a northern native temperate grassland in central Alberta, Canada, over a two-year period.

ISBN: 9780494605103Subjects--Topical Terms:

894284
Climate Change.

Biogeochemical cycling and microbial communities in native grasslands: Responses to climate change and defoliation.
LDR:02565nam 2200277 4500 001 1398777
005 20110915090223.5
008 130515s2010 ||||||||||||||||| ||eng d
020 $a 9780494605103
035 $a (UMI)AAINR60510
035 $a AAINR60510
040 $a UMI $c UMI
100 1 $a Attaeian, Behnaz. $3 1677678
245 1 0 $a Biogeochemical cycling and microbial communities in native grasslands: Responses to climate change and defoliation.
300 $a 217 p.
500 $a Source: Dissertation Abstracts International, Volume: 71-05, Section: B, page: 2903.
502 $a Thesis (Ph.D.)--University of Alberta (Canada), 2010.
520 $a Ongoing climate change has emerged as a major scientific challenge in the current century. Grassland ecosystems are considered net carbon (C) sinks to mitigate climate change. However, they are in turn, influenced by climate change and management practices, providing feedback to climate change via soil microbial community and biogeochemical fluxes. In this thesis, I examined the impact of warming, altered precipitation, and defoliation on soil microbial composition and function, C and N dynamics, and fluxes in soil respiration (CO2), nitrous oxide (N2O) and methane (CH 4), together with other belowground ecosystem functions, within two ecosites in a northern native temperate grassland in central Alberta, Canada, over a two-year period.
520 $a Fungi-to-bacteria ratio was not affected by climatic parameters or defoliation, indicating a high degree of resistance in the below ground community to the treatments imposed. However, C substrate utilization was influenced by warming and defoliation, as was soil microbial biomass. In contrast, soil respiration (or C loss) was not. Soil respiration acclimatized rather quickly to warming, and N2O and CH4 effluxes showed minor responses to warming at both ecosites, regardless of defoliation. These results suggest warming is unlikely to lead to positive climate change feedback due to soil-based responses, regardless of ongoing land use. However, altered precipitation (+/- 50%) demonstrated greater impacts on C and N fluxes relative to warming and defoliation. Increased precipitation stimulated soil C loss to the atmosphere, potentially generating positive feedback for climatic warming in this northern temperate grassland.
590 $a School code: 0351.
650 4 $a Climate Change. $3 894284
650 4 $a Biogeochemistry. $3 545717
650 4 $a Natural Resource Management. $3 676989
690 $a 0404
690 $a 0425
690 $a 0528
710 2 $a University of Alberta (Canada). $3 626651
773 0 $t Dissertation Abstracts International $g 71-05B.
790 $a 0351
791 $a Ph.D.
792 $a 2010
856 4 0 $u http://pqdd.sinica.edu.tw/twdaoapp/servlet/advanced?query=NR60510