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- W3196636616 abstract "Abstract In this study, the first in situ static‐chamber measurements were conducted at coastal Antarctica tundra for CHCl 3 fluxes, which showed that CHCl 3 was naturally emitted from the Antarctic tundra at 35 ± 27 nmol m −2 d −1 , comparable to other reported important natural sources. Significantly, enhanced CHCl 3 emission rates (66 ± 20 nmol m −2 d −1 ) were observed from ornithogenic soil on the island populated with penguins, which was rich in organic matter and halides coming from penguin excrements. It is estimated that Antarctic tundra emits up to 0.1 Gg CHCl 3 per year, which is an important source for regional atmospheric CHCl 3 . Laboratory‐based incubations suggested that organic carbon and chlorine inputs by penguins may stimulate O 2 dependent microbial‐mediated CHCl 3 emission from the Antarctic tundra, and all tundra soils showed the maximum CHCl 3 emission at 4°C. The strength of this CHCl 3 source is also expected to change in response to Antarctic warming." @default.
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- W3196636616 date "2021-09-14" @default.
- W3196636616 modified "2023-10-09" @default.
- W3196636616 title "Chloroform (CHCl<sub>3</sub>) Emissions From Coastal Antarctic Tundra" @default.
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- W3196636616 doi "https://doi.org/10.1029/2021gl093811" @default.
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