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Thursday, October 24, 2013

Top 3 Bachelor/ettes of Microbial Soil Science Speed Dating!

Soils Speed Dating-Top 3 Bachelor/ettes

1. #14-Red alder alters community level microbial function in conifer forests of the Pacific Northwest, USA
a. This research is needed to explore the impacts of different forest types on soil health and microbial activity. The presence of certain trees (Red alder) or lack of them, rather, can have significant impact on the productivity of microbes in the soil, and therefore the soil itself.
b. Soil samples were analyzed for microbial activity and other productivity measures in pure alder stands, pure conifer stands, and mixed conifer-alder stands in the Pacific Northwest.
c. The study found that microbial activity and other soil productivity measures were significantly greater in the pure alder and mixed alder-conifer stands.
d. I’ve seen this research coming for a long time, or rather hoped to see it come out, as I grew up in the Willamette valley and watched over the years as mixed oak, alder, and maple forests were clear cut and then replanted as pure conifer stands. This study provides reasoning to refrain from using this practice, and that in order to maintain productive, healthy soil and enzymes within it, managers should replant mixed deciduous-conifer stands instead of planting monoculture conifer stands.

2. #18- Soil Moisture is the major factor influencing microbial community structure and enzyme activities across seven biogeoclimatic zones in western Canada
a. Because microbial activity partially determines productivity and fertility of a soil, it is important to know what they prefer for habitat and under which conditions they thrive. Other studies demonstrate the effect of different microbes on the soil, but this study examined the impact of soil factors on microbe communities.
b. Intact soil samples were collected from a variety of sites throughout western Canada, and analyzed for a wide array of soil characteristics.
c. Conclusions were made that soil moisture content is the single most important factor in determining microbial biomass and productivity within a soil.
d. Implications of this study extend upon an already known truth; soil health is connected to the amount of moisture it receives. Furthermore, different soil enzymes occur in different forest types, and in turn influence the activity of those different soil types. It was concluded that the right combination of temperature and precipitation provides habitat for the most desirable (highest activity level) enzymes.

3. #15- Response of microbial community composition and function to soil climate change
a. As climate change progresses it is important to understand variances in the ability of different soils to acclimate to such changes. This study looked at the ability of both sub-oak canopy soils and open grassland soils to withstand changes in localized climate. As forests are cleared and grasslands are plowed for agriculture, it should be known to what extent the critical functions in these soils will be affected.
b. Soil cores were taken from open grasslands and moved into sub-oak canopy environment, and cores from sub-oak canopy locations were transferred to open grasslands. For up to two years, both cores were regularly evaluated with microbial analyses tests to see how each was responding to the switch.
c. The study concluded that grassland soils are much more resistant to a change in their environment, and sub-canopy soils experience much higher levels of stress and an overall decrease in function.
d. These findings imply that considerations should be made about the impacts of not only the atmospheric and hydrologic impacts of land clearing, but also the effect land clearing will have on the health of the soil and its ability to function at its full ecological potential. Perhaps instead of clearing a forest in its entirety for pasture, leave a number of broad canopy trees in order to protect the soil from sudden climatic change and allow it to maintain it’s microbial community structure.

          All of these studies made an impact on the way I think about land use changes and their subsequent effects on long-term soil activity, productivity, and general health. I have long wondered about significantly altering plant community compositions and what implications this held for soil composition and function. However, I haven’t given as much thought to the effects of climate change on soil communities, as most direct observations involving climate change are experienced above ground, in plant and animal populations. These studies make me consider more in depth the decisions of land managers and what possible threats they pose to soil productivity, both short and long term. Many of these microbial communities can be easily wiped out by significant moisture or temperature regime changes, such as during a forest clearing or damming event. However, the reestablishment and resiliency to change in these microbial populations cannot keep up with our rapid land use changes. What will the future effects of these changes be on soil communities and their health on a long-term scale? Is it possible that the very basis of our ecological function as a planet is at stake because of how we are treating our wild soils? If decomposition falters or is detrimentally impacted to the point where it cannot keep up with death…where will that leave us in a hundred, or a thousand years? I ruminate…

Sunday, October 6, 2013

Blog # 2: Nitrogen Cycling



Denitrification

Plants require nitrogen in order to grow and prosper, and we require plants, in one way or another, to do the same. Soil provides adequate habitat for anaerobic bacteria that are capable of transforming atmospheric nitrogen into molecular nitrogen (N2), which is a usable form of nitrogen as far as plants are concerned (atmospheric nitrogen is not able to be absorbed by plants). The cycling of nitrogen is an ecological service because plants transform energy from the sun into usable energy for all organisms on earth, and without any organisms, there would be no ecology. Microorganisms (including nitrogen fixing anaerobic bacteria) are dependent on soil for habitat; in fact they are just one part of what makes soil, soil. Therefore denitrification is a process of soil itself. Because of soil, microorganisms can exist, because of these microorganisms, plants can exist, and because plants exist, the rest of us can too. Hoorah.

Tuesday, October 1, 2013

Introduction-Blog #1


Hello fellow soils students! My name on the books is Kirsten Williams, however I go by Hillary, which is my middle name. I grew up in a tiny town called Lorane, which is located roughly 23 miles southwest of Eugene, OR. Lorane has a population of a little less than 1000, and is made up of ranchers, loggers, vineyard workers, and hippies. My family fell under the last category. I am a natural resource/management option major, and I have been a senior for the last year and a half, but I will actually be graduating this June (finally). I am taking this class because it fits into my plan, but I chose it because I became a self-proclaimed soil geek after taking intro to soils in Corvallis with the infamous James Cassidy. Wild land soils is particularly interesting to me because I hope to work in the water/watershed management field at some point in my career, and the ecosystem services wild soils provide is largely integrated into that realm of resource management. The most interesting place I have looked at a soil would have to be either Glacier Nat’l Park or on Kauai and Maui. Glacier is astounding because you can see the evolution of the soil and the many layers of time within the rock. On the other end of the spectrum are the very young red rock soils of the Hawaiian Islands, which intrigue me due to their workable and fertile properties. See y'all in class!