Publication Date:
2012-04-13
Description:
Aims Ecosystem carbon models often require accurate net ecosystem exchange of CO 2 (NEE) light-response parameters, which can be derived from the Michaelis–Menten equation. These parameters include maximum net ecosystem exchange (NEE max ), apparent quantum use efficiency ( α ) and daytime ecosystem respiration rate ( R e ). However, little is known about the effects of land conversion between steppe and cropland on these parameters, especially in semi-arid regions. To understand how these parameters vary in responses to biotic and abiotic factors under land conversions, seasonal variation of light-response parameters were evaluated for a steppe and a cropland of Inner Mongolia, China, during three consecutive years (2006–08) with different precipitation amounts. Methods NEE was measured over a steppe and a cropland in Duolun, Inner Mongolia, China, using the eddy covariance technique, and NEE light-response parameters (NEE max , α and R e ) were derived using the Michaelis–Menten model. Biophysical regulations of these parameters were evaluated using a stepwise regression analysis. Important Findings The maximum absolute values of NEE max occurred in the meteorological regimes of 15°C ≤ T a 〈 25°C, vapor pressure deficit (VPD) 〈 1 KPa and 0.21 m 3 m – 3 ≤ volumetric soil water content at 10 cm (SWC) 〈 0.28 m 3 m – 3 for both the steppe and the cropland ecosystems. The variations of α and R e showed no regular variation pattern in different T air , VPD and SWC regimes. Under the same regime of T air , VPD and SWC, the cropland had higher absolute values of NEE max than the steppe. Canopy conductance and leaf area index (LAI) were dominant drivers for variations in NEE light-response parameters of the steppe and the cropland. The seasonal variation of NEE light-response parameters followed the variation of LAI for two ecosystems. The peak values of all light-response parameters for the steppe and the cropland occurred from July to August. The values of NEE light-response parameters (NEE max , α and R e ) were lower in the driest year (2007). Seasonally averaged NEE light-response parameters for the cropland surpassed those for the steppe. Land conversion from steppe to cropland enhanced NEE light-response parameters during the plant growing period. These results will have significant implications for improving the models on regional NEE variation under climate change and land-use change scenarios.
Print ISSN:
1752-993X
Electronic ISSN:
1752-9921
Topics:
Biology
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