Zobrazeno 1 - 10
of 397
pro vyhledávání: '"Davidson EA"'
Publikováno v:
In Current Opinion in Environmental Sustainability November 2014 9-10:46-54
Publikováno v:
In Current Opinion in Environmental Sustainability November 2014 9-10:1-8
Autor:
Thompson, RL, Lassaletta, L, Patra, PK, Wilson, C, Wells, KC, Gressent, A, Koffi, EN, Chipperfield, MP, Winiwarter, W, Davidson, EA, Tian, H, Canadell, JG
Nitrous oxide (N2O) is the third most important long-lived GHG and an important stratospheric ozone depleting substance. Agricultural practices and the use of N-fertilizers have greatly enhanced emissions of N2O. Here, we present estimates of N2O emi
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=core_ac_uk__::b123d1e929ab2ffd0e7043378c60645c
https://eprints.whiterose.ac.uk/154482/1/N2O_trends_revision2_v1_clean.pdf
https://eprints.whiterose.ac.uk/154482/1/N2O_trends_revision2_v1_clean.pdf
Publikováno v:
Sihi, D; Davidson, EA; Chen, M; Savage, KE; Richardson, AD; Keenan, TF; et al.(2018). Merging a mechanistic enzymatic model of soil heterotrophic respiration into an ecosystem model in two AmeriFlux sites of northeastern USA. Agricultural and Forest Meteorology, 252, 155-166. doi: 10.1016/j.agrformet.2018.01.026. UC Berkeley: Retrieved from: http://www.escholarship.org/uc/item/5bm2b861
© 2018 Elsevier B.V. Heterotrophic respiration (Rh), microbial processing of soil organic matter to carbon dioxide (CO2), is a major, yet highly uncertain, carbon (C) flux from terrestrial systems to the atmosphere. Temperature sensitivity of Rh is
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=dedup_wf_001::4dea2bec199d5730af69910136f37b8e
https://escholarship.org/uc/item/5bm2b861
https://escholarship.org/uc/item/5bm2b861
Autor:
Wieder, WR, Allison, SD, Davidson, EA, Georgiou, K, Hararuk, O, He, Y, Hopkins, F, Luo, Y, Smith, MJ, Sulman, B, Todd-Brown, K, Wang, YP, Xia, J, Xu, X
Publikováno v:
Global Biogeochemical Cycles, vol 29, iss 10
Wieder, WR; Allison, SD; Davidson, EA; Georgiou, K; Hararuk, O; He, Y; et al.(2015). Explicitly representing soil microbial processes in Earth system models. Global Biogeochemical Cycles, 29(10), 1782-1800. doi: 10.1002/2015GB005188. UC Irvine: Retrieved from: http://www.escholarship.org/uc/item/19d1n3jt
Wieder, WR; Allison, SD; Davidson, EA; Georgiou, K; Hararuk, O; He, Y; et al.(2015). Explicitly representing soil microbial processes in Earth system models. Global Biogeochemical Cycles, 29(10), 1782-1800. doi: 10.1002/2015GB005188. UC Irvine: Retrieved from: http://www.escholarship.org/uc/item/19d1n3jt
©2015. American Geophysical Union. All Rights Reserved. Microbes influence soil organic matter decomposition and the long-term stabilization of carbon (C) in soils. We contend that by revising the representation of microbial processes and their inte
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=dedup_wf_001::1aa430b2c3cdd3d8c197135478432d81
https://escholarship.org/uc/item/19d1n3jt
https://escholarship.org/uc/item/19d1n3jt
Autor:
Massad, TJ, Balch, JK, Davidson, EA, Brando, PM, Mews, CL, Porto, P, Quintino, RM, Vieira, SA, Junior, BHM, Trumbore, SE
Publikováno v:
Massad, TJ; Balch, JK; Davidson, EA; Brando, PM; Mews, CL; Porto, P; et al.(2013). Interactions between repeated fire, nutrients, and insect herbivores affect the recovery of diversity in the southern Amazon.. Oecologia, 172(1), 219-229. doi: 10.1007/s00442-012-2482-x. UC Irvine: Retrieved from: http://www.escholarship.org/uc/item/67r5z37v
Surface fires burn extensive areas of tropical forests each year, altering resource availability, biotic interactions, and, ultimately, plant diversity. In transitional forest between the Brazilian cerrado (savanna) and high stature Amazon forest, we
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=od_______325::07ee5541004b52d0cbeea5e4a20fd9c8
http://www.escholarship.org/uc/item/67r5z37v
http://www.escholarship.org/uc/item/67r5z37v
Autor:
Davidson, EA, De Araújo, AC, Artaxo, P, Balch, JK, Brown, IF, Bustamante, MMC, Coe, MT, Defries, RS, Keller, M, Longo, M, Munger, JW, Schroeder, W, Soares-Filho, BS, Souza, CM, Wofsy, SC
Publikováno v:
Nature, vol 483, iss 7388
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=od_______325::b070266fa3e981798469b722fe961a63
https://escholarship.org/uc/item/4fj508sx
https://escholarship.org/uc/item/4fj508sx
Publikováno v:
Davidson, EA; Savage, KE; Trumbore, SE; & Borken, W. (2007). Erratum: Vertical partitioning of CO2 production within a temperate forest soil (Global Change Biology vol. 12 (944-956)). Global Change Biology, 13(4), 922. doi: 10.1111/j.1365-2486.2007.01335.x. UC Irvine: Retrieved from: http://www.escholarship.org/uc/item/88g0x067
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=od_______325::ff77bb14625a3028bc5996da2839a81b
http://www.escholarship.org/uc/item/88g0x067
http://www.escholarship.org/uc/item/88g0x067
Publikováno v:
Davidson, EA; Savage, KE; Trumbore, SE; & Borken, W. (2006). Vertical partitioning of CO2production within a temperate forest soil. Global Change Biology, 12(6), 944-956. doi: 10.1111/j.1365-2486.2005.01142.x. UC Irvine: Retrieved from: http://www.escholarship.org/uc/item/12k087qs
The major driving factors of soil CO2production - substrate supply, temperature, and water content - vary vertically within the soil profile, with the greatest temporal variations of these factors usually near the soil surface. Several studies have d
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=od_______325::3cac185d2d82ec79bfcc6055ccf23020
http://www.escholarship.org/uc/item/12k087qs
http://www.escholarship.org/uc/item/12k087qs
Autor:
Angert A, Barkan E, Barnett B, Brugnoli E, Davidson EA, Fessenden J, Maneepong S, Panapitukkul N, Randerson JT, Savage K, Yakir D, Luz B
Publikováno v:
Global biogeochemical cycles 17 (2003): 1089–1099.
info:cnr-pdr/source/autori:Angert A, Barkan E, Barnett B, Brugnoli E, Davidson EA, Fessenden J, Maneepong S, Panapitukkul N, Randerson JT, Savage K, Yakir D, Luz B/titolo:Contribution of soil respiration in tropical, temperate, and boreal forests to the 18O enrichment of atmospheric O2/doi:/rivista:Global biogeochemical cycles/anno:2003/pagina_da:1089/pagina_a:1099/intervallo_pagine:1089–1099/volume:17
info:cnr-pdr/source/autori:Angert A, Barkan E, Barnett B, Brugnoli E, Davidson EA, Fessenden J, Maneepong S, Panapitukkul N, Randerson JT, Savage K, Yakir D, Luz B/titolo:Contribution of soil respiration in tropical, temperate, and boreal forests to the 18O enrichment of atmospheric O2/doi:/rivista:Global biogeochemical cycles/anno:2003/pagina_da:1089/pagina_a:1099/intervallo_pagine:1089–1099/volume:17
The O-18 content of atmospheric O-2 is an important tracer for past changes in the biosphere. Its quantitative use depends on knowledge of the discrimination against O-18 associated with the various O-2 consumption processes. Here we evaluated, for t
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=cnr_________::b5dd9e59a38c913a61231a6d5edfa9ae
https://publications.cnr.it/doc/10610
https://publications.cnr.it/doc/10610