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Items: 6

1.

Export of ice nucleating particles from a watershed.

Larsen JA, Conen F, Alewell C.

R Soc Open Sci. 2017 Aug 30;4(8):170213. doi: 10.1098/rsos.170213. eCollection 2017 Aug.

2.

Ice nucleation active particles are efficiently removed by precipitating clouds.

Stopelli E, Conen F, Morris CE, Herrmann E, Bukowiecki N, Alewell C.

Sci Rep. 2015 Nov 10;5:16433. doi: 10.1038/srep16433.

3.

Bioprecipitation: a feedback cycle linking earth history, ecosystem dynamics and land use through biological ice nucleators in the atmosphere.

Morris CE, Conen F, Alex Huffman J, Phillips V, Pöschl U, Sands DC.

Glob Chang Biol. 2014 Feb;20(2):341-51. doi: 10.1111/gcb.12447. Epub 2013 Nov 26.

PMID:
24399753
4.

δ15N natural abundance may directly disclose perturbed soil when related to C:N ratio.

Conen F, Yakutin MV, Carle N, Alewell C.

Rapid Commun Mass Spectrom. 2013 May 30;27(10):1101-4. doi: 10.1002/rcm.6552.

PMID:
23592114
5.

δ15N natural abundance in permafrost soil indicates impact of fire on nitrogen cycle.

Conen F, Yakutin MV, Puchnin AN, Leifeld J, Alewell C.

Rapid Commun Mass Spectrom. 2011 Mar 15;25(5):661-4. doi: 10.1002/rcm.4911.

PMID:
21290453
6.

Fractionation factors for stable isotopes of N and O during N2O reduction in soil depend on reaction rate constant.

Vieten B, Blunier T, Neftel A, Alewell C, Conen F.

Rapid Commun Mass Spectrom. 2007;21(6):846-50.

PMID:
17294513

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