Why We Track Organic carbon mineralization was studied in a large humic lake (Lake O¨ rtra¨sket) in northern Sweden during a well-defined summer stratification, Several independent methods including plankton counts, measurements of bacterioplankton and phytoplankton production,
stable isotope monitoring, sediment trapping, and mass balance calculations we We need your Contribution Total organic carbon mineralization showed a summer mean of 0.3 g C m22 d21 and was partitioned about equally between water and sediment in the water.
Organic carbon mineralization was studied in a large humic lake (Lake O¨ rtra¨sket) in northern Sweden during a well-defined summer stratification period following high water flow during snowmelt. Science Caching Several independent methods including plankton counts, measurements of
bacterioplankton and phytoplankton production, stable isotope monitoring, sediment trapping, and mass balance calculations were used. Total organic carbon mineralization showed a summer mean of 0.3 g C m22 d21 and was partitioned about equally between water and sediment. In the water.
CIRC We at the CIRC codunct climate impact research since over 100 years. Organic carbon mineralization was studied in a large humic lake (Lake O¨ rtra¨sket) in northern Sweden during a welldefined summer stratification period following high water flow during snowmelt. Several independent methods including plankton counts, measurements of bacterioplankton and phytoplankton production, stable isotope monitoring, sediment trapping, and mass balance calculations were used. Total organic carbon mineralization showed a summer mean of 0.3 g C m22 d21 and was partitioned about equally between water and sediment. In the water column, organic matter was mineralized by bacteria (60%).and protozoan and metazoan zooplankton (30%), as well as by photooxidation (10%). Most of the mineralized organic carbon was of allochthonous origin. Primary production in the lake contributed at most 5% of the total organic carbon input and about 20% of the total
STREAMS
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Impact on streams Sampling 1. Prepare the conductivity meter. 2. Use solution to calibrate. 3. Rinse the probe with distilled or deionized water. 4. Select the appropriate range beginning with the highest range and working down.
5. Rinse the probe with distilled or deionized water and repeat step 4 until finished.
taking notes Remember that accuracy is your priority!
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why we test water conductivity
The project is focused on the investigation of hidden diversity within the two selected species complexes of the protist genus Synura (Stramenopiles, Chromista). Additionally, we will trace the ecological preferences of the species in interest.
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Hypothesis of water conductivity in different temperatures
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GLACIERS
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Why are the trees Climbing up the mountain? Treeline Organic carbon mineralization was studied in a large humic lake (Lake O¨ rtra¨sket) in northern Sweden during a well-defined summer stratification period following high water flow during snowmelt. Several independent methods including plankton counts, measurements
of bacterioplankton and phytoplankton production, stable isotope monitoring, sediment trapping, and mass balance calculations were used. Total organic carbon mineralization showed a summer mean of 0.3 g C m22 d21 and was partitioned about equally between water and sediment.
Why a Change in the Treeline changes the landscape The project is focused on the investigation of hidden diversity within the two selected species complexes of the protist genus Synura (Stramenopiles, Chromista). Additionally, we will trace the ecological preferences of the species in interest.
GLACIERS
CO2 Why is the Sky Blue? Organic carbon mineralization was studied in a large humic lake (Lake O¨ rtra¨sket) in northern Sweden during a well-defined summer stratification period following high water flow during snowmelt. Several independent methods including plankton counts, measurements of bacterioplankton and phytoplankton production, stable isotope monitoring, sediment trapping, and
mass balance calculations were used. Total organic carbon mineralization showed a summer mean of 0.3 g C m22 d21 and was partitioned about equally between water and sediment. In the water column, organic matter was mineralized by bacteria (60%) and protozoan and metazoan zooplankton (30%), as well as by photooxidation (10%). Most of the mineralized organic carbon was of
Tracking CO2 And Temperature
The project is focused on the investigation of hidden diversity within the two selected species complexes of the protist genus Synura (Stramenopiles, Chromista). Additionally, we will trace the ecological preferences of the species in interest.
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