Matches in SemOpenAlex for { <https://semopenalex.org/work/W4206050037> ?p ?o ?g. }
- W4206050037 abstract "Abstract Cold ecosystems in regions of high‐latitude and altitude with vast stores of soil organic carbon suffer strong freeze‐thaw cycles, which can greatly affect soil CO 2 release. However, on the Tibetan Plateau, where altitude is >4,000 m, it remains unknown how freeze‐thaw processes regulate CO 2 production across the soil profile. In this study, we used the gradient method to explore impacts of freeze‐thaw processes on depthwise soil CO 2 production in an alpine steppe. We found almost all soil CO 2 was produced in the root‐zone layer (<30 cm), while the root‐free layer (>30 cm) frequently alternated between being a source and sink of CO 2 and thus acted largely as a buffer. The surface layer (0–15 cm) and subsurface layer (15–30 cm) had a similar CO 2 production rate in the thawed period. However, during the freezing‐frozen‐thawing period, the subsurface layer consistently functioned as a weak CO 2 source, although parts were trapped in frozen soil, resulting in a weaker CO 2 sink in the surface layer. Soil CO 2 production in subsurface layer is thus more sensitive to temperature variability compared with surface layer. Furthermore, our results suggest water content plays a more important role than temperature in regulating soil CO 2 production. For the first time, our data set reveals the vertical production of CO 2 within the seasonally frozen soils on the Tibetan Plateau, which will benefit understanding of belowground carbon processes and modeling of soil CO 2 release in the region." @default.
- W4206050037 created "2022-01-25" @default.
- W4206050037 creator A5032828615 @default.
- W4206050037 creator A5032898271 @default.
- W4206050037 creator A5048440698 @default.
- W4206050037 creator A5070895238 @default.
- W4206050037 date "2022-01-01" @default.
- W4206050037 modified "2023-09-26" @default.
- W4206050037 title "Depthwise Soil CO <sub>2</sub> Production Is Controlled by Freeze‐Thaw Processes in a Tibetan Alpine Steppe" @default.
- W4206050037 cites W1210931142 @default.
- W4206050037 cites W1505543708 @default.
- W4206050037 cites W1965358300 @default.
- W4206050037 cites W1967095068 @default.
- W4206050037 cites W1967892189 @default.
- W4206050037 cites W1968317338 @default.
- W4206050037 cites W1968565544 @default.
- W4206050037 cites W1968801125 @default.
- W4206050037 cites W1969056482 @default.
- W4206050037 cites W1969764600 @default.
- W4206050037 cites W1973998243 @default.
- W4206050037 cites W1976984800 @default.
- W4206050037 cites W1991060563 @default.
- W4206050037 cites W1992387731 @default.
- W4206050037 cites W1996342844 @default.
- W4206050037 cites W1998154286 @default.
- W4206050037 cites W1998830422 @default.
- W4206050037 cites W2012558448 @default.
- W4206050037 cites W2015789373 @default.
- W4206050037 cites W2018907779 @default.
- W4206050037 cites W2026749811 @default.
- W4206050037 cites W2034727817 @default.
- W4206050037 cites W2039571901 @default.
- W4206050037 cites W2039764743 @default.
- W4206050037 cites W2043390548 @default.
- W4206050037 cites W2053156815 @default.
- W4206050037 cites W2059554936 @default.
- W4206050037 cites W2067198255 @default.
- W4206050037 cites W2069850703 @default.
- W4206050037 cites W2073644661 @default.
- W4206050037 cites W2074769503 @default.
- W4206050037 cites W2077723871 @default.
- W4206050037 cites W2083857556 @default.
- W4206050037 cites W2085965018 @default.
- W4206050037 cites W2087453069 @default.
- W4206050037 cites W2089940084 @default.
- W4206050037 cites W2092094003 @default.
- W4206050037 cites W2093519717 @default.
- W4206050037 cites W2095245387 @default.
- W4206050037 cites W2098627306 @default.
- W4206050037 cites W2102729778 @default.
- W4206050037 cites W2105172241 @default.
- W4206050037 cites W2106445377 @default.
- W4206050037 cites W2106776098 @default.
- W4206050037 cites W2111398301 @default.
- W4206050037 cites W2113594455 @default.
- W4206050037 cites W2122133520 @default.
- W4206050037 cites W2123438286 @default.
- W4206050037 cites W2124685322 @default.
- W4206050037 cites W2125671750 @default.
- W4206050037 cites W2128317583 @default.
- W4206050037 cites W2128324299 @default.
- W4206050037 cites W2132997281 @default.
- W4206050037 cites W2134501245 @default.
- W4206050037 cites W2140236466 @default.
- W4206050037 cites W2174069807 @default.
- W4206050037 cites W2174960450 @default.
- W4206050037 cites W2206439460 @default.
- W4206050037 cites W2207837310 @default.
- W4206050037 cites W2290308683 @default.
- W4206050037 cites W2328871881 @default.
- W4206050037 cites W2534439660 @default.
- W4206050037 cites W2554403554 @default.
- W4206050037 cites W2587837857 @default.
- W4206050037 cites W2591086493 @default.
- W4206050037 cites W2612845390 @default.
- W4206050037 cites W2780522730 @default.
- W4206050037 cites W2889400510 @default.
- W4206050037 cites W2889727732 @default.
- W4206050037 cites W2891537950 @default.
- W4206050037 cites W2896524764 @default.
- W4206050037 cites W2900111710 @default.
- W4206050037 cites W2903289733 @default.
- W4206050037 cites W2940219602 @default.
- W4206050037 cites W2953122562 @default.
- W4206050037 cites W2964681705 @default.
- W4206050037 cites W2987596107 @default.
- W4206050037 cites W2989688343 @default.
- W4206050037 cites W2997409821 @default.
- W4206050037 cites W2997947152 @default.
- W4206050037 cites W308501013 @default.
- W4206050037 cites W3092352293 @default.
- W4206050037 cites W3105161351 @default.
- W4206050037 cites W3113136507 @default.
- W4206050037 cites W3130923633 @default.
- W4206050037 cites W3132150883 @default.
- W4206050037 cites W647257035 @default.
- W4206050037 doi "https://doi.org/10.1029/2021jg006678" @default.
- W4206050037 hasPublicationYear "2022" @default.
- W4206050037 type Work @default.
- W4206050037 citedByCount "2" @default.