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Die Messung von Tagesgängen der Kohlenstoffdioxid-Flüsse mit manuellen Hauben startet vor Sonnenaufgang (Großes Moor bei Gifhorn, 04:45 Uhr).
Die Messung von Tagesgängen der Kohlenstoffdioxid-Flüsse mit manuellen Hauben startet vor Sonnenaufgang (Großes Moor bei Gifhorn, 04:45 Uhr).
Institut für

AK Agrarklimaschutz

Referierte Publikationen von Lena Rohe

  1. 0

    Rohe L, Anderson T-H, Flessa H, Goeske A, Lewicka-Szczebak D, Wrage-Mönnig N, Well R (2021) Comparing modified substrate-induced respiration with selective inhibition (SIRIN) and N2O isotope approaches to estimate fungal contribution to denitrification in three arable soils under anoxic conditions. Biogeosciences 18(15):4629-4650, DOI:10.5194/bg-18-4629-2021

    https://literatur.thuenen.de/digbib_extern/dn063919.pdf

  2. 1

    Rohe L, Apelt B, Vogel H-J, Well R, Wu G-M, Schlüter S (2021) Denitrification in soil as a function of oxygen availability at the microscale. Biogeosciences 18(3):1185-1201, DOI:10.5194/bg-18-1185-2021

    https://literatur.thuenen.de/digbib_extern/dn063355.pdf

  3. 2

    Rohe L, Oppermann T, Well R, Horn MA (2020) Nitrite induced transcription of p450nor during denitrification by Fusarium oxysporum correlates with the production of N2O with a high 15N site preference. Soil Biol Biochem 151:108043, DOI:10.1016/j.soilbio.2020.108043

  4. 3

    Well R, Buchen C, Köster JR, Lewicka-Szczebak D, Rohe L, Senbayram M, Wu D (2019) A critique of the paper "Estimate of bacterial and fungal N2O production processes after crop residue input and fertilizer application to an agricultural field by 15N isotopomer analysis", by Yamamoto et al. (2017), Soil Biology & Biochemistry 108, 9–16. Soil Biol Biochem 135:450-451, DOI:10.1016/j.soilbio.2018.06.008

  5. 4

    Jung M-Y, Gwak J-H, Rohe L, Giesemann A, Kim J-G, Well R, Madsen EL, Herbold CW, Wagner M, Rhee S-K (2019) Indications for enzymatic denitrification to N2O at low pH in an ammonia-oxidizing archaeon. ISME J 13:2633-2638, DOI:10.1038/s41396-019-0460-6

    https://literatur.thuenen.de/digbib_extern/dn061442.pdf

  6. 5

    Rohe L, Well R, Lewicka-Szczebak D (2017) Use of oxygen isotopes to differentiate between nitrous oxide produced by fungi or bacteria during denitrification. Rapid Comm Mass Spectrometry 31(16):1297-1312, DOI:10.1002/rcm.7909

  7. 6

    Rohe L, Anderson T-H, Braker G, Flessa H, Giesemann A, Lewicka-Szczebak D, Wrage-Mönnig N, Well R (2014) Dual isotope and isotopomer signatures of nitrous oxide from fungal denitrification - a pure culture study. Rapid Comm Mass Spectrometry 28:1893-1903, DOI:10.1002/rcm.6975

  8. 7

    Rohe L, Anderson T-H, Braker G, Flessa H, Giesemann A, Wrage-Mönnig N, Well R (2014) Fungal oxygen exchange between denitrification intermediates and water. Rapid Comm Mass Spectrometry 28(4):377-384, DOI:10.1002/rcm.6790

  9. 8

    Lewicka-Szczebak D, Well R, Giesemann A, Rohe L, Wolf U (2013) An enhanced technique for automated determination of 15N signatures of N2, (N2+N2O) and N2O in gas samples. Rapid Comm Mass Spectrometry 27(13):1548-1558, DOI:10.1002/rcm.6605

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