The Characteristics and Seasonal Variation of Methane Fluxes From an Alpine Wetland in the Qinghai Lake watershed, China

Wetlands ◽  
2021 ◽  
Vol 41 (5) ◽  
Author(s):  
Fangtao Wu ◽  
Shengkui Cao ◽  
Guangchao Cao ◽  
Kelong Chen ◽  
Changhui Peng
Author(s):  
Guang-Zhao Han ◽  
Sheng-Kui Cao ◽  
Guang-Chao Cao ◽  
Ke-Long Chen ◽  
Jing Zhang ◽  
...  

2011 ◽  
Vol 10 ◽  
pp. 2426-2430 ◽  
Author(s):  
Zhu Jinfu ◽  
Chen Kelong ◽  
Wu Yanpeng ◽  
Cao Guangchao ◽  
Cao Shengkui ◽  
...  

2014 ◽  
Vol 937 ◽  
pp. 565-570
Author(s):  
Ji Ming Wang ◽  
Ke Long Chen ◽  
Xin Zhang ◽  
Zheng Xia Luo

Using FieldSpec ® 4 Hi-Res portable coverings spectrometer, we have measured the main vegetation and siol reflectance based on different habitats:Surface water swamping meadow, a seasonal water swamping beach, wet beach without of water and sandy in the little Park Lake, East of the Qinghai Lake and analyzed the spectral differences. The results show that: Soil moisture is one of the important factors that affect reflectivity. Under the premise of similar other soil properties, soil moisture and reflectivity shows a negative correlation with each other. 350-1000nm wavelength range is ideal to distinguish vegetation and soil. Due to the presence of water absorption bands, within 1000-1300nm the spectrum derivative of soil and vegetation has a strong similarity, but still can be used to identify the spectrum of vegetation and soil. In addition to sandy habitats, vegetation and soil spectrum has a strong similarity in the 1300-2500nm wavelength range, it is more tolerance translation will confuse the two bands, the spectrum has a strong similarity in the range of 1300-2500nm, so it is relatively easy to confuse the two spectrum.


Author(s):  
Jing Zhang ◽  
Sheng-Kui Cao ◽  
Guang-Chao Cao ◽  
Ke-Long Chen ◽  
Guang-Zhao Han ◽  
...  

2017 ◽  
Vol 76 (5) ◽  
Author(s):  
Shengkui Cao ◽  
Guangchao Cao ◽  
Qi Feng ◽  
Guangzhao Han ◽  
Yangyang Lin ◽  
...  

Author(s):  
Yang-Yang Lin ◽  
Sheng-Kui Cao ◽  
Guang-Chao Cao ◽  
Ke-Long Chen ◽  
Jing Zhang ◽  
...  

Author(s):  
Palingamoorthy Gnanamoorthy ◽  
S. Chakraborty ◽  
R. Nagarajan ◽  
R. Ramasubramanian ◽  
V. Selvam ◽  
...  

2019 ◽  
Vol 9 (1) ◽  
Author(s):  
Jun-Fu Zhao ◽  
Shu-Shi Peng ◽  
Meng-Ping Chen ◽  
Guan-Ze Wang ◽  
Yi-Bin Cui ◽  
...  

AbstractAlthough tropical forest soils contributed substantially global soil methane uptake, observations on soil methane fluxes in tropical forests are still sparse, especially in Southeast Asia, leading to large uncertainty in the estimation of global soil methane uptake. Here, we conducted two-year (from Sep, 2016 to Sep, 2018) measurements of soil methane fluxes in a lowland tropical forest site in Hainan island, China. At this tropical forest site, soils were substantial methane sink, and average annual soil methane uptake was estimated at 2.00 kg CH4-C ha−1 yr−1. The seasonality of soil methane uptake showed strong methane uptake in the dry season (−1.00 nmol m−2 s−1) and almost neutral or weak soil methane uptake in the wet season (−0.24 nmol m−2 s−1). The peak soil methane uptake rate was observed as −1.43 nmol m−2 s−1 in February, 2018, the driest and coolest month during the past 24 months. Soil moisture was the dominant controller of methane fluxes, and could explain 94% seasonal variation of soil methane fluxes. Soil temperature could not enhance the explanation of seasonal variation of soil methane fluxes on the top of soil moisture. A positive relationship between soil methane uptake and soil respiration was also detected, which might indicate co-variation in activities of methanotroph and roots and/or microbes for soil heterotrophic respiration. Our study highlights that tropical forests in this region acted as a methane sink.


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