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You are here: Abacus-IPY >> Work Packages
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Section Contents |
WP3: Soil/plant flux measurements (Leader: Dr R Baxter + Ineson, Mencuccini, Williams, Huntley)We will provide to WP7 high temporal resolution of C exchange of the key tundra-dwarf-shrub and forest understorey communities through diurnal cycles at different times of year, coupled with, where relevant, concomitant measurements of CO2 exchange of branches of the tree Betula. We propose to employ a series of integrated campaigns of measurements, combining multiplexed automatic clear plastic CO2 chambers (after Bubier et al, 2002) with an automatic multiplexed branch-bag approach (Rayment et al, 2002). Particular attention will be paid to the key ‘shoulder’ seasons of the winter-spring transition and autumn-winter transition (H3a,b). In addition, the automated chamber approach has been used very successfully previously (Bubier et al, 2002) to measure net ecosystem exchange of C (NEE) during the snow-covered season. Winter fluxes will be measured on a campaign basis of 1-2 weeks in winter, making measurements every 3 hours by sampling changes in headspace concentrations of CO2. We will pay particular attention to the period of spring thaw when freezing and thawing events can lead to large changes in build-up and release of CO2 and is an important and often poorly represented period of the annual CO2 exchange budget. We will provide suitable fine-scale temporal resolution of C and water exchange across the whole range of dominant vegetation types, and across boundaries between types, at key times of the yearly cycle. This will be achieved by deployment of large 1m x 1m portable chamber systems that are flexible in operation height (Williams et al., in press), linked to a LiCOR 6400 portable IRGA, for use over a range of canopies of dwarf shrub (e.g. Betula nana and Salix species ca. 50 cm and 75-100 cm tall; requiring no permanent collars, and therefore avoiding ‘damage artefacts’). Multiple rapid assessments of light response curves of NEE, over the different vegetation canopies comprising the tundra, and forest, understorey will be made along with light intensity, prevailing air and soil temperature, and soil moisture. We will provide fine-scale spatial and temporal measurements of soil respiration from northern forest and tundra soils. This will be addressed by campaign deployments of a state-of-the-art multiplexed automated soil CO2 flux system, comprising 2 x 12 multiplexed automated chambers (developed by Ineson and Heinemeyer, University of York, in collaboration with LiCOR, inc. USA), and a similar single ‘roving’ unit for obtaining good spatial coverage within and at boundaries of vegetation units. Deliverables Tasks |
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