9 June, 2001
As anywhere else the weekends are not as hectic work wise as weekdays. This weekend promises to be slower than most. We are still getting instruments ready and projects organized. Glen tells us this will not be true for all weekends however! We stayed in the lab catching up on reading and writing. After lunch, Spring and I went out to the site to return 4 cells to the soil moisture measuring instrament. Out in the field most all instruments are kept inside 10 or 20-gallon igloo coolers. The instruments put out heat when operating, the chests keep the heat in and this prevents the electronics from freezing. Most instruments are run on simple batteries, from flashlight to 12 volt. In our case we are close enough to electric cables that we have a direct electrical connection
Soil moisture measurements are important when determining CO2 flux. Picture soil, which is composed of separate grains of material, which fit tightly together, like marbles in a cup. Between each grain is a space, tiny but it's there. When soil moisture is high these spaces are filled with water. With water in the spaces gas exchanges cannot take place. Now, dry out that soil and you leave the spaces open and gases, like CO2, can fill those spaces. When plants grow the roots take up O2 and give off CO2 during respiration. Bacterias in the soil, whose main function is to decompose materials, also produces CO2. Thus, with these two CO2 sources, the gases build up in the soil and can potentially be released into the atmosphere. What's going on in the pore spaces is an important variable to consider when measuring CO2 flux. Right now, because of the spring melt, soil moisture is high but as the summer season progresses there will be measurable changes.
Walking back to the truck I took a picture of an area of uplifted tundra. This is a landscape form found in the arctic referred to as a "tundra boil". They are caused by the constant freezing and thawing of the layers under the surface. When the water, in the active layer freezes it expands, pushing the surface upward. Cracks develop in the ground surface. Thawing allows more water to seep into these surface cracks and then the area freezes once again pushing the surface layer up higher. Eventually the lower layers are brought to the surface and the soils are turned (cryo-turbation). From a distance the tundra has a flat look to it but on walking on it you see how hummocky (hilly) it really is. The surface rolls very gently for hundreds of miles till it reaches the foothills of the Brooks Range, which is about 150 miles south. In the arctic the permafrost layer is the primary sculptor or the landscape with alternating cycles of freezing and thawing its tool.
On the way back to the lab we stopped of to take some pictures of the whalebones that are on display all around the area. The native people, the Inupiat, hunt the bowhead whale and it is not uncommon to see head and rib bones decorating the landscape. Standing next to these you get the idea of how big these marine mammals are and the skill and energy it must take to capture and kill them.
Contact the TEA in the field at .
If you cannot connect through your browser, copy the TEA's e-mail address in the "To:" line of your favorite e-mail package.