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Ecosystem carbon and water budgets u...
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Lund, Christopher Paul.
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Ecosystem carbon and water budgets under elevated atmospheric carbon dioxide concentration in two California grasslands.
紀錄類型:
書目-語言資料,印刷品 : Monograph/item
正題名/作者:
Ecosystem carbon and water budgets under elevated atmospheric carbon dioxide concentration in two California grasslands./
作者:
Lund, Christopher Paul.
面頁冊數:
161 p.
附註:
Adviser: Christopher B. Field.
Contained By:
Dissertation Abstracts International63-01B.
標題:
Biogeochemistry. -
電子資源:
http://pqdd.sinica.edu.tw/twdaoapp/servlet/advanced?query=3040040
ISBN:
0493533524
Ecosystem carbon and water budgets under elevated atmospheric carbon dioxide concentration in two California grasslands.
Lund, Christopher Paul.
Ecosystem carbon and water budgets under elevated atmospheric carbon dioxide concentration in two California grasslands.
- 161 p.
Adviser: Christopher B. Field.
Thesis (Ph.D.)--Stanford University, 2002.
Stomatal conductance and photosynthesis play central roles in regulating the fluxes of water (H<sub>2</sub>O) and carbon (C) between the land surface and the atmosphere. Anthropogenically driven increases in atmospheric carbon dioxide (CO<sub>2</sub>) concentration may have a significant impact on these fluxes by decreasing stomatal conductance and increasing photosynthesis. Here, using a combination of gas-exchange and modeling results, I describe the effects of elevated atmospheric CO<sub>2</sub> concentration (720 ppmv) on ecosystem water and carbon budgets in serpentine and sanstone annual grasslands. Averaged across grasslands, daily evapotranspiration (ET) decreased by an average of 0.53 mm H<sub>2</sub>O day<super>−1</super> under elevated CO<sub>2</sub> during the winter and spring months. Decreases in ET were accompanied by increases in soil moisture and deep drainage. During the summer, early season water savings resulted in an average ET increase of 0.12 mm H<sub> 2</sub>O day<super>−1</super> under elevated CO<sub>2</sub>. On an annual basis, simulation results show that ET decreased by an average of 26.5 mm H<sub>2</sub>O y<super>−1</super>. For the net ecosystem CO<sub>2</sub> exchange analyses, I used soil CO<sub>2</sub> flux measurements in conjunction with a soil CO<sub>2</sub> transport model to remove the bias introduced by chamber pressurization. In the sandstone grassland, net ecosystem production (NEP) increased from 55.6 g C m<super>−2</super> y<super>−1</super> under ambient CO<sub>2</sub> to 59.6 g C m<super>−2</super> y<super> −1</super> under elevated CO<sub>2</sub>, a difference of 4.0 g C m<super> −2</super>. Annual canopy net photosynthesis (A<sub>n</sub>) increased under elevated CO<sub>2</sub> by 35.8 g C m<super>−2</super> y<super> −1</super>, but the bulk of this increase was returned to the atmosphere via root and heterotrophic respiration. Canopy A<sub>n</sub> decreased under elevated CO<sub>2</sub> early in the growing season, an observation that may reflect nitrogen limitation. These results suggest that future increases in atmospheric CO<sub>2</sub> concentration will significantly reduce evapotranspiration but have only minimal effects on ecosystem C uptake.
ISBN: 0493533524Subjects--Topical Terms:
545717
Biogeochemistry.
Ecosystem carbon and water budgets under elevated atmospheric carbon dioxide concentration in two California grasslands.
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Stomatal conductance and photosynthesis play central roles in regulating the fluxes of water (H<sub>2</sub>O) and carbon (C) between the land surface and the atmosphere. Anthropogenically driven increases in atmospheric carbon dioxide (CO<sub>2</sub>) concentration may have a significant impact on these fluxes by decreasing stomatal conductance and increasing photosynthesis. Here, using a combination of gas-exchange and modeling results, I describe the effects of elevated atmospheric CO<sub>2</sub> concentration (720 ppmv) on ecosystem water and carbon budgets in serpentine and sanstone annual grasslands. Averaged across grasslands, daily evapotranspiration (ET) decreased by an average of 0.53 mm H<sub>2</sub>O day<super>−1</super> under elevated CO<sub>2</sub> during the winter and spring months. Decreases in ET were accompanied by increases in soil moisture and deep drainage. During the summer, early season water savings resulted in an average ET increase of 0.12 mm H<sub> 2</sub>O day<super>−1</super> under elevated CO<sub>2</sub>. On an annual basis, simulation results show that ET decreased by an average of 26.5 mm H<sub>2</sub>O y<super>−1</super>. For the net ecosystem CO<sub>2</sub> exchange analyses, I used soil CO<sub>2</sub> flux measurements in conjunction with a soil CO<sub>2</sub> transport model to remove the bias introduced by chamber pressurization. In the sandstone grassland, net ecosystem production (NEP) increased from 55.6 g C m<super>−2</super> y<super>−1</super> under ambient CO<sub>2</sub> to 59.6 g C m<super>−2</super> y<super> −1</super> under elevated CO<sub>2</sub>, a difference of 4.0 g C m<super> −2</super>. Annual canopy net photosynthesis (A<sub>n</sub>) increased under elevated CO<sub>2</sub> by 35.8 g C m<super>−2</super> y<super> −1</super>, but the bulk of this increase was returned to the atmosphere via root and heterotrophic respiration. Canopy A<sub>n</sub> decreased under elevated CO<sub>2</sub> early in the growing season, an observation that may reflect nitrogen limitation. These results suggest that future increases in atmospheric CO<sub>2</sub> concentration will significantly reduce evapotranspiration but have only minimal effects on ecosystem C uptake.
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http://pqdd.sinica.edu.tw/twdaoapp/servlet/advanced?query=3040040
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