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Spatiotemporal Monitoring of Soil CO<sub>2</sub> Efflux in a Subtropical Forest during the Dry Season Based on Field Observations and Remote Sensing Imagery
oleh: Tao Chen, Zhenwu Xu, Guoping Tang, Xiaohua Chen, Hong Fang, Hao Guo, Ye Yuan, Guoxiong Zheng, Liangliang Jiang, Xiangyu Niu
Format: | Article |
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Diterbitkan: | MDPI AG 2021-09-01 |
Deskripsi
The CO<sub>2</sub> efflux from forest soil (FCO<sub>2</sub>) is one of the largest components of the global carbon cycle. Accurate estimation of FCO<sub>2</sub> can help us better understand the carbon cycle in forested areas and precisely predict future climate change. However, the scarcity of field-measured FCO<sub>2</sub> data in the subtropical forested area greatly limits our understanding of FCO<sub>2</sub> dynamics at regional and global scales. This study used an automatic cavity ring-down spectrophotometer (CRDS) analyzer to measure FCO<sub>2</sub> in a typical subtropical forest of southern China in the dry season. We found that the measured FCO<sub>2</sub> at two experimental areas experienced similar temporal trends in the dry season and reached the minima around December, whereas the mean FCO<sub>2</sub> differed apparently across the two areas (9.05 vs. 5.03 g C m<sup>−2</sup> day<sup>−1</sup>) during the dry season. Moreover, we found that both abiotic (soil temperature and moisture) and biotic (vegetation productivity) factors are significantly and positively correlated, respectively, with the FCO<sub>2</sub> variation during the study period. Furthermore, a machine-learning random forest model (RF model) that incorporates remote sensing data is developed and used to predict the FCO<sub>2</sub> pattern in the subtropical forest, and the topographic effects on spatiotemporal patterns of FCO<sub>2</sub> were further investigated. The model evaluation indicated that the proposed model illustrated high prediction accuracy for the training and testing dataset. Based on the proposed model, the spatiotemporal patterns of FCO<sub>2</sub> in the forested watershed that encloses the two monitoring sites were mapped. Results showed that the spatial distribution of FCO<sub>2</sub> is obviously affected by topography: the high FCO<sub>2</sub> values mainly occur in relatively high altitudinal areas, in slopes of 10–25°, and in sunny slopes. The results emphasized that future studies should consider topographical effects when simulating FCO<sub>2</sub> in subtropical forests. Overall, our study unraveled the spatiotemporal variations of FCO<sub>2</sub> and their driving factors in a subtropical forest of southern China in the dry season, and demonstrated that the proposed RF model in combination with remote sensing data can be a useful tool for predicting FCO<sub>2</sub> in forested areas, particularly in subtropical and tropical forest ecosystems.