GLORIA

GEOMAR Library Ocean Research Information Access

feed icon rss

Ihre E-Mail wurde erfolgreich gesendet. Bitte prüfen Sie Ihren Maileingang.

Leider ist ein Fehler beim E-Mail-Versand aufgetreten. Bitte versuchen Sie es erneut.

Vorgang fortführen?

Exportieren
Filter
Publikationsart
Verlag/Herausgeber
Erscheinungszeitraum
  • 1
    ISSN: 1573-515X
    Schlagwort(e): carex ; methane oxidation ; methyl fluoride ; peatlands ; rhizosphere
    Quelle: Springer Online Journal Archives 1860-2000
    Thema: Chemie und Pharmazie , Geologie und Paläontologie
    Notizen: Abstract Rhizospheric methane oxidation was evaluated at a Carex (spp.) dominated fen in Alberta, Canada overthree growing seasons. Aerobic incubations of bulkpeat and live roots in the laboratory show a clearassociation between active methane oxidizing bacteriaand the rhizosphere. Aerobic incubations also show anoxidation potential that far exceeds methaneproduction potential measured in the laboratory. Quantitative estimates of how this oxidation potentialis expressed in situ depend strongly on which of twocommon approaches are used. (1) Subtracting in situmethane emission rates from methane production ratesmeasured in the laboratory with anaerobic incubationssuggest that methane oxidation may attenuate emissionsby 58 to 92%. (2) Applying the inhibitor methylfluoride (CH3F) to whole plants in situ suggestmethane oxidation attenuates emissions by less than20% seasonally. The production minus emissiontechnique likely overestimates methane oxidationbecause methane production measured via anaerobicincubations in the laboratory are probablyoverestimates. Oxidation percentages measured byCH3F were greatest early in the growing seasonwhen emission rates were low and fell to almostnondetectable levels as emission rates peaked in latesummer. Estimates provided by the CH3F techniquewere generally in better agreement with estimates ofoxidation based on a stable isotope mass balance(0–34%) determined in a companion study (Popp et al. 1999).
    Materialart: Digitale Medien
    Standort Signatur Einschränkungen Verfügbarkeit
    BibTip Andere fanden auch interessant ...
  • 2
    Publikationsdatum: 2017-10-17
    Beschreibung: In the last couple of years remote sensing data have shown large areas of wet snow in the Southern part of the Greenland ice sheet. These melt features are attributed to the overall warming trend. Persistent warming implies changes in the firn layer as well. Even in areas of the dry snow zone one can observe sporadically a few ice lenses within the firn column indicating refrozen meltwater from warm events in the past. In our contribution we want to close the gap between investigations of firn cores drilled in the 70's and the observational record of remote sensing data over the last decade in South Greenland. The focus lies on firn of the dry snow zone which is sensitive against changes in a warming atmosphere and cold enough to prevent a longway percolation path of meltwater to several firn layers. To this end we had drilled two 45m-long firn cores at the former drilling sites of DYE3 (65°11'N, 43°49'W) and South Dome (SD) (63°32'N, 44°34'W) during a aircraft-supported field campaign 2012. The retrieved 3inch-firn core segments of 1m length are measured by a X-ray-scanning routine with the means of the core-scale AWI-ICE-CT. The 2d-density fields are calculated and allow to distinguish between refreezing meltwater and compacted firn. The depth-scales are converted to time-scales by using DEP (dielectric profiling) and (in case of DYE3) discrete sampled d18O measurements. Number density of melt layers and relative amount of melt show an synchronized behavior with an general increase over the last 30 years. Local maxima are observed in both sites at around 6-9m and 25m at DYE3 and 5-8m, 22m and 40m at SD.
    Repository-Name: EPIC Alfred Wegener Institut
    Materialart: Conference , notRev
    Format: application/pdf
    Standort Signatur Einschränkungen Verfügbarkeit
    BibTip Andere fanden auch interessant ...
  • 3
    Publikationsdatum: 2021-10-22
    Beschreibung: We report high resolution measurements of the stable isotope ratios of ancient ice (δ18O, δD) from the North Greenland Eemian deep ice core (NEEM, 77.45° N, 51.06° E). The record covers the period 8–130 ky b2k (y before 2000) with a temporal resolution of ≈0.5 and 7 y at the top and the bottom of the core respectively and contains important climate events such as the 8.2 ky event, the last glacial termination and a series of glacial stadials and interstadials. At its bottom part the record contains ice from the Eemian interglacial. Isotope ratios are calibrated on the SMOW/SLAP scale and reported on the GICC05 (Greenland Ice Core Chronology 2005) and AICC2012 (Antarctic Ice Core Chronology 2012) time scales interpolated accordingly. We also provide estimates for measurement precision and accuracy for both δ18O and δD.
    Repository-Name: EPIC Alfred Wegener Institut
    Materialart: Article , isiRev
    Standort Signatur Einschränkungen Verfügbarkeit
    BibTip Andere fanden auch interessant ...
Schließen ⊗
Diese Webseite nutzt Cookies und das Analyse-Tool Matomo. Weitere Informationen finden Sie hier...