2019
DOI: 10.1016/j.scitotenv.2018.10.057
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Responses of soil respiration to rainfall addition in a desert ecosystem: Linking physiological activities and rainfall pattern

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Cited by 24 publications
(9 citation statements)
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“…Therefore, a single deluge was able to increase seasonal soil respiration, but earlier deluges (Early and Mid) caused a greater increase than a deluge later in the season. Such dynamic temporal responses have been found in other arid and semi‐arid ecosystems, with larger soil respiration increases following an early‐season rain pulse than a late‐season one (Chou, Silver, Jackson, Thompson, & Allen‐Diaz, 2008; Song et al., 2012; Wang et al., 2019). This dampened response to late‐season deluge events could be attributed to decreased root activity as plants begin to senesce towards the end of the growing season (Knight, 1973; Parton et al., 2012).…”
Section: Discussionmentioning
confidence: 60%
“…Therefore, a single deluge was able to increase seasonal soil respiration, but earlier deluges (Early and Mid) caused a greater increase than a deluge later in the season. Such dynamic temporal responses have been found in other arid and semi‐arid ecosystems, with larger soil respiration increases following an early‐season rain pulse than a late‐season one (Chou, Silver, Jackson, Thompson, & Allen‐Diaz, 2008; Song et al., 2012; Wang et al., 2019). This dampened response to late‐season deluge events could be attributed to decreased root activity as plants begin to senesce towards the end of the growing season (Knight, 1973; Parton et al., 2012).…”
Section: Discussionmentioning
confidence: 60%
“…Third, the significant differences in SWC and AN can also result in variations in R S among the different sites. The multiple stepwise linear regression analysis revealed that the concentration of SWC was of much greater importance than AN on bacterial community composition, which suggested that SWC is very likely to be the restricting factor in the metabolic process in dry and semi‐dry ecosystems (Zhang et al ., 2015; Wang et al ., 2019).…”
Section: Discussionmentioning
confidence: 99%
“…Soil respiration (SR), mainly composed of soil autotrophic respiration and soil heterotrophic respiration (Yu et al, 2017; Zhang, Li, et al, 2019), is the largest source of carbon flux from the terrestrial ecosystem to the atmosphere (Bond‐Lamberty & Allison, 2010; Liu et al, 2016; Wang et al, 2019). And its dynamics will be critically important for the accurate prediction of the potential for carbon sequestration in terrestrial ecosystems (Qu et al, 2019; Zhang, Zhao, et al, 2019).…”
Section: Introductionmentioning
confidence: 99%