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Marshland conversion to cropland in northeast China from 1950 to 2000 reduced the greenhouse effect
Author(s) -
HUANG YAO,
SUN WENJUAN,
ZHANG WEN,
YU YONGQIANG,
SU YANHUA,
SONG CHANGCHUN
Publication year - 2010
Publication title -
global change biology
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 4.146
H-Index - 255
eISSN - 1365-2486
pISSN - 1354-1013
DOI - 10.1111/j.1365-2486.2009.01976.x
Subject(s) - greenhouse gas , nitrous oxide , environmental science , marsh , wetland , methane , paddy field , environmental engineering , environmental chemistry , agronomy , chemistry , ecology , biology , organic chemistry
It has been well recognized that converting wetlands to cropland results in loss of soil organic carbon (SOC), while less attention was paid to concomitant changes in methane (CH 4 ) and nitrous oxide (N 2 O) emissions. Using datasets from the literature and field measurements, we investigated loss of SOC and emissions of CH 4 and N 2 O due to marshland conversion in northeast China. Analysis of the documented crop cultivation area indicated that 2.91 Mha of marshland were converted to cropland over the period 1950–2000. Marshland conversion resulted in SOC loss of ∼240 Tg and introduced ∼1.4 Tg CH 4 and ∼138 Gg N 2 O emissions in the cropland, while CH 4 emissions reduced greatly in the marshland, cumulatively ∼28 Tg over the 50 years. Taking into account the loss of SOC and emissions of CH 4 and N 2 O, the global warming potential (GWP) at a 20‐year time horizon was estimated to be ∼180 Tg CO 2 _eq. yr −1 in the 1950s and ∼120 Tg CO 2 _eq. yr −1 in the 1990s, with a ∼33% reduction. When calculated at 100‐year time horizon, the GWP was ∼73 Tg CO 2 _eq. yr −1 in the 1950s and ∼58 Tg CO 2 _eq. yr −1 in the 1990s, with a ∼21% reduction. It was concluded that marshland conversion to cropland in northeast China reduced the greenhouse effect as far as GWP is concerned. This reduction was attributed to a substantial decrease in CH 4 emissions from the marshland. An extended inference is that the declining growth rate of atmospheric CH 4 since the 1980s might be related to global loss of wetlands, but this connection needs to be confirmed.