Soil CO2 efflux and soil carbon balance of a tropical rubber plantation
Natural rubber is a valuable source of income in many tropical countries and rubber trees are increasingly planted in tropical areas, where they contribute to land-use changes that impact the global carbon cycle. However, little is known about the carbon balance of these plantations. We studied the...
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Published in | Advances in ecological research Vol. 28; no. 6; pp. 969 - 979 |
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Main Authors | , , , , , , , |
Format | Journal Article |
Language | English |
Published |
Tokyo
Springer Japan
01.11.2013
Springer Blackwell Publishing Ltd Elsevier |
Subjects | |
Online Access | Get full text |
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Summary: | Natural rubber is a valuable source of income in many tropical countries and rubber trees are increasingly planted in tropical areas, where they contribute to land-use changes that impact the global carbon cycle. However, little is known about the carbon balance of these plantations. We studied the soil carbon balance of a 15-year-old rubber plantation in Thailand and we specifically explored the seasonal dynamic of soil CO
2
efflux (
F
S
) in relation to seasonal changes in soil water content (
W
S
) and soil temperature (
T
S
), assessed the partitioning of
F
S
between autotrophic (
R
A
) and heterotrophic (
R
H
) sources in a root trenching experiment and estimated the contribution of aboveground and belowground carbon inputs to the soil carbon budget. A multiplicative model combining both
T
S
and
W
S
explained 58 % of the seasonal variation of
F
S
. Annual soil CO
2
efflux averaged 1.88 kg C m
−2
year
−1
between May 2009 and April 2011 and
R
A
and
R
H
accounted for respectively 63 and 37 % of
F
S
, after corrections of
F
S
measured on trenched plots for root decomposition and for difference in soil water content. The 4-year average annual aboveground litterfall was 0.53 kg C m
−2
year
−1
while a conservative estimate of belowground carbon input into the soil was much lower (0.17 kg C m
−2
year
−1
). Our results highlighted that belowground processes (root and rhizomicrobial respiration and the heterotrophic respiration related to belowground carbon input into the soil) have a larger contribution to soil CO
2
efflux (72 %) than aboveground litter decomposition. |
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Bibliography: | SourceType-Scholarly Journals-1 ObjectType-Feature-1 content type line 14 ObjectType-Article-1 ObjectType-Feature-2 content type line 23 |
ISSN: | 0912-3814 0065-2504 1440-1703 2163-582X |
DOI: | 10.1007/s11284-013-1079-0 |