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fast response open path ch 4 analyzer  (LI-COR)


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    LI-COR fast response open path ch 4 analyzer
    Electrical Resistivity Tomography (ERT) transects transformed to VWC estimates for the NSY E–W transect A ( a ) and N–S transect D ( b ) profiles are shown together with observed methane (CH 4 ) fluxes within 5 m (transparency scaled by distance from ERT line) and predicted flux classifications (purple ribbon plot) at continuous locations along each profile.
    Fast Response Open Path Ch 4 Analyzer, supplied by LI-COR, used in various techniques. Bioz Stars score: 95/100, based on 199 PubMed citations. ZERO BIAS - scores, article reviews, protocol conditions and more
    https://www.bioz.com/product/open+path+ch4+analyzer/pmc11258132-263-35-41?v=LI-COR
    Average 95 stars, based on 199 article reviews
    fast response open path ch 4 analyzer - by Bioz Stars, 2026-07
    95/100 stars

    Images

    1) Product Images from "Upland Yedoma taliks are an unpredicted source of atmospheric methane"

    Article Title: Upland Yedoma taliks are an unpredicted source of atmospheric methane

    Journal: Nature Communications

    doi: 10.1038/s41467-024-50346-5

    Electrical Resistivity Tomography (ERT) transects transformed to VWC estimates for the NSY E–W transect A ( a ) and N–S transect D ( b ) profiles are shown together with observed methane (CH 4 ) fluxes within 5 m (transparency scaled by distance from ERT line) and predicted flux classifications (purple ribbon plot) at continuous locations along each profile.
    Figure Legend Snippet: Electrical Resistivity Tomography (ERT) transects transformed to VWC estimates for the NSY E–W transect A ( a ) and N–S transect D ( b ) profiles are shown together with observed methane (CH 4 ) fluxes within 5 m (transparency scaled by distance from ERT line) and predicted flux classifications (purple ribbon plot) at continuous locations along each profile.

    Techniques Used: Tomography, Transformation Assay

    a , summer (BH1) and b , winter (BH6) cores. In the winter core, the surface frost layer was ~50 cm thick, and the top of permafrost was observed at 700 cm belowground. Error bars for CH 4 and CO 2 concentrations and their δ 13 C values are the standard deviation (SD) of two technical replicates. Data for mcrA and pmoA absolute gene expression are presented as mean ± SEM of three technical replicates. Source data are provided as a Source Data file.
    Figure Legend Snippet: a , summer (BH1) and b , winter (BH6) cores. In the winter core, the surface frost layer was ~50 cm thick, and the top of permafrost was observed at 700 cm belowground. Error bars for CH 4 and CO 2 concentrations and their δ 13 C values are the standard deviation (SD) of two technical replicates. Data for mcrA and pmoA absolute gene expression are presented as mean ± SEM of three technical replicates. Source data are provided as a Source Data file.

    Techniques Used: Standard Deviation, Expressing

    Air and soil temperature ( a ), methane (CH 4 ) flux and atmospheric pressure ( b ), and carbon dioxide (CO 2 ) flux and soil moisture expressed as volumetric water content at 15 cm depth ( c ).
    Figure Legend Snippet: Air and soil temperature ( a ), methane (CH 4 ) flux and atmospheric pressure ( b ), and carbon dioxide (CO 2 ) flux and soil moisture expressed as volumetric water content at 15 cm depth ( c ).

    Techniques Used:



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    Image Search Results


    Electrical Resistivity Tomography (ERT) transects transformed to VWC estimates for the NSY E–W transect A ( a ) and N–S transect D ( b ) profiles are shown together with observed methane (CH 4 ) fluxes within 5 m (transparency scaled by distance from ERT line) and predicted flux classifications (purple ribbon plot) at continuous locations along each profile.

    Journal: Nature Communications

    Article Title: Upland Yedoma taliks are an unpredicted source of atmospheric methane

    doi: 10.1038/s41467-024-50346-5

    Figure Lengend Snippet: Electrical Resistivity Tomography (ERT) transects transformed to VWC estimates for the NSY E–W transect A ( a ) and N–S transect D ( b ) profiles are shown together with observed methane (CH 4 ) fluxes within 5 m (transparency scaled by distance from ERT line) and predicted flux classifications (purple ribbon plot) at continuous locations along each profile.

    Article Snippet: The eddy-covariance instrumentation included a 3-D sonic anemometer (CSAT-3B; Campbell Scientific Instruments, Logan, Utah, USA), an open-path infrared gas analyzer for CO 2, water, and energy fluxes (LI-7500DS IRGA; LI-COR, Lincoln, Nebraska, USA), and a fast-response open-path CH 4 analyzer (LI-7700; LI-COR, Lincoln, Nebraska, USA).

    Techniques: Tomography, Transformation Assay

    a , summer (BH1) and b , winter (BH6) cores. In the winter core, the surface frost layer was ~50 cm thick, and the top of permafrost was observed at 700 cm belowground. Error bars for CH 4 and CO 2 concentrations and their δ 13 C values are the standard deviation (SD) of two technical replicates. Data for mcrA and pmoA absolute gene expression are presented as mean ± SEM of three technical replicates. Source data are provided as a Source Data file.

    Journal: Nature Communications

    Article Title: Upland Yedoma taliks are an unpredicted source of atmospheric methane

    doi: 10.1038/s41467-024-50346-5

    Figure Lengend Snippet: a , summer (BH1) and b , winter (BH6) cores. In the winter core, the surface frost layer was ~50 cm thick, and the top of permafrost was observed at 700 cm belowground. Error bars for CH 4 and CO 2 concentrations and their δ 13 C values are the standard deviation (SD) of two technical replicates. Data for mcrA and pmoA absolute gene expression are presented as mean ± SEM of three technical replicates. Source data are provided as a Source Data file.

    Article Snippet: The eddy-covariance instrumentation included a 3-D sonic anemometer (CSAT-3B; Campbell Scientific Instruments, Logan, Utah, USA), an open-path infrared gas analyzer for CO 2, water, and energy fluxes (LI-7500DS IRGA; LI-COR, Lincoln, Nebraska, USA), and a fast-response open-path CH 4 analyzer (LI-7700; LI-COR, Lincoln, Nebraska, USA).

    Techniques: Standard Deviation, Expressing

    Air and soil temperature ( a ), methane (CH 4 ) flux and atmospheric pressure ( b ), and carbon dioxide (CO 2 ) flux and soil moisture expressed as volumetric water content at 15 cm depth ( c ).

    Journal: Nature Communications

    Article Title: Upland Yedoma taliks are an unpredicted source of atmospheric methane

    doi: 10.1038/s41467-024-50346-5

    Figure Lengend Snippet: Air and soil temperature ( a ), methane (CH 4 ) flux and atmospheric pressure ( b ), and carbon dioxide (CO 2 ) flux and soil moisture expressed as volumetric water content at 15 cm depth ( c ).

    Article Snippet: The eddy-covariance instrumentation included a 3-D sonic anemometer (CSAT-3B; Campbell Scientific Instruments, Logan, Utah, USA), an open-path infrared gas analyzer for CO 2, water, and energy fluxes (LI-7500DS IRGA; LI-COR, Lincoln, Nebraska, USA), and a fast-response open-path CH 4 analyzer (LI-7700; LI-COR, Lincoln, Nebraska, USA).

    Techniques: