2020
DOI: 10.1016/j.geoderma.2020.114636
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Impact of differences in soil temperature on the desert carbon sink

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Cited by 27 publications
(19 citation statements)
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“…Although the real-time temperature in the stratosphere was below 0 • C, cyanobacterial crusts were able to absorb heat from solar radiation, thus increasing the soil temperature. Studies have shown that soil microorganisms in the Qinghai-Tibetan Plateau, Taklimakan Desert, Mu Us Desert, and Tengger Desert still have aerobic respiration activity under −10 • C~0 • C in winter [42][43][44][45]. Although the stratospheric environment was different from that on the ground, our results show that crusts microorganisms exhibited activity at a certain period of time during stratospheric exposure.…”
Section: Damage Degree and Tolerance Mechanisms Of Cyanobacterial Crustsmentioning
confidence: 51%
“…Although the real-time temperature in the stratosphere was below 0 • C, cyanobacterial crusts were able to absorb heat from solar radiation, thus increasing the soil temperature. Studies have shown that soil microorganisms in the Qinghai-Tibetan Plateau, Taklimakan Desert, Mu Us Desert, and Tengger Desert still have aerobic respiration activity under −10 • C~0 • C in winter [42][43][44][45]. Although the stratospheric environment was different from that on the ground, our results show that crusts microorganisms exhibited activity at a certain period of time during stratospheric exposure.…”
Section: Damage Degree and Tolerance Mechanisms Of Cyanobacterial Crustsmentioning
confidence: 51%
“…The model calculates the total regional carbon stock through four carbon pools based on land use data. The carbon pool data used in this study were monitored from relevant experimental studies 6 , 59 ; the sandy areas were listed separately because the recent studies have determined that the deserts in Xinjiang have some carbon sink capacity 60 . In this study, the data most suitable for the arid zone were selected, and the carbon density with multiple reference values were averaged to obtain the carbon density table for this study (Table 2 ).…”
Section: Methodsmentioning
confidence: 99%
“…All three types of NKEFAs can achieve co-benefits of CS and EQ, and similar to Liu et al (2020), the soil conservation type has the greatest improvement effect. In contrast, the windbreak sand-fixation type only positively contributes to CS, probably because deserts, as an important part of terrestrial ecosystems, can sequester large amounts of carbon dioxide and play a key role as carbon sinks (Yang et al, 2020). However, the windbreak sand-fixation type is generally located in fragile ecosystems with high desertification and severe grassland degradation, with limited environmental benefits and still has a long way to go.…”
Section: Localization and Precision In The Management Of Nkefasmentioning
confidence: 99%