Zobrazeno 1 - 10
of 212
pro vyhledávání: '"G. M. Santos"'
Application of the ECT9 protocol for radiocarbon-based source apportionment of carbonaceous aerosols
Publikováno v:
Atmospheric Measurement Techniques, Vol 14, Pp 3481-3500 (2021)
Carbonaceous aerosol is mainly composed of organic carbon (OC) and elemental carbon (EC). Both OC and EC originate from a variety of emission sources. Radiocarbon (14C) analysis can be used to apportion bulk aerosol, OC, and EC into their sources. Ho
Externí odkaz:
https://doaj.org/article/3b1776b35a4648f1b08781d60e76690c
Autor:
T. W. Chan, L. Huang, K. Banwait, W. Zhang, D. Ernst, X. Wang, J. G. Watson, J. C. Chow, M. Green, C. I. Czimczik, G. M. Santos, S. Sharma, K. Jones
Publikováno v:
Atmospheric Measurement Techniques, Vol 12, Pp 4543-4560 (2019)
Carbonaceous aerosol is a major contributor to the total aerosol load and being monitored by diverse measurement approaches. Here, 10 years (2005–2015) of continuous carbonaceous aerosol measurements collected at the Centre of Atmospheric Research
Externí odkaz:
https://doaj.org/article/4d999089048a46eca1819ade75e1a2c5
Autor:
A. Alexandre, J. Balesdent, P. Cazevieille, C. Chevassus-Rosset, P. Signoret, J.-C. Mazur, A. Harutyunyan, E. Doelsch, I. Basile-Doelsch, H. Miche, G. M. Santos
Publikováno v:
Biogeosciences, Vol 13, Iss 5, Pp 1693-1703 (2016)
In the rhizosphere, the uptake of low-molecular-weight carbon (C) and nitrogen (N) by plant roots has been well documented. While organic N uptake relative to total uptake is important, organic C uptake is supposed to be low relative to the plant's C
Externí odkaz:
https://doaj.org/article/c72c6ee790724006ba6fe0a17d472436
Autor:
P. E. Reyerson, A. Alexandre, A. Harutyunyan, R. Corbineau, H. A. Martinez De La Torre, F. Badeck, L. Cattivelli, G. M. Santos
Publikováno v:
Biogeosciences, Vol 13, Iss 4, Pp 1269-1286 (2016)
Plant biosilica particles (phytoliths) contain small amounts of carbon called phytC. Based on the assumptions that phytC is of photosynthetic origin and a closed system, claims were recently made that phytoliths from several agriculturally important
Externí odkaz:
https://doaj.org/article/4c6d9dca0adc4fe2a50434cfe18dab04
Autor:
G. O. Mouteva, S. M. Fahrni, G. M. Santos, J. T. Randerson, Y.-L. Zhang, S. Szidat, C. I. Czimczik
Publikováno v:
Atmospheric Measurement Techniques, Vol 8, Iss 9, Pp 3729-3743 (2015)
Aerosol source apportionment remains a critical challenge for understanding the transport and aging of aerosols, as well as for developing successful air pollution mitigation strategies. The contributions of fossil and non-fossil sources to organic c
Externí odkaz:
https://doaj.org/article/5f108808cf1e4a258ed54b3c67cdd428
Autor:
A. Alexandre, I. Basile-Doelsch, T. Delhaye, D. Borshneck, J. C. Mazur, P. Reyerson, G. M. Santos
Publikováno v:
Biogeosciences, Vol 12, Iss 3, Pp 863-873 (2015)
Phytoliths contain occluded organic compounds called phytC. Recently, phytC content, nature, origin, paleoenvironmental meaning and impact in the global C cycle have been the subject of increasing debate. Inconsistencies were fed by the scarcity of i
Externí odkaz:
https://doaj.org/article/723f02dd571a425ebc3b9e37a5f1a01b
Publikováno v:
Biogeosciences, Vol 9, Iss 5, Pp 1873-1884 (2012)
Plants absorb and transport silicon (Si) from soil, and precipitation of Si within the living plants results in micrometric amorphous biosilica particles known as phytoliths. During phytolith formation, a small amount of carbon (2) via photosynthesis
Externí odkaz:
https://doaj.org/article/cfe2cd018a6547aa9afef39249e5547a
Autor:
Ana C. O. Barbosa, Dilson S. Rocha, Glaucia C. B. Silva, Miguel G. M. Santos, Luciana R. Camillo, Paulo H. G. A. de Oliveira, Aline A. Cavalari, Marcio G. C. Costa
Publikováno v:
Physiology and Molecular Biology of Plants. 29:159-172
Publikováno v:
Fluvial Megafans on Earth and Mars ISBN: 9781108525923
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::38ccd2079416e41032eb5c81fe7922c8
https://doi.org/10.1017/9781108525923.009
https://doi.org/10.1017/9781108525923.009
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