Thursday, October 20, 2011
Lake Michigan
Thursday, October 6, 2011
Ocumulgee National Park
On Wednesday we went to visit the Ocumulgee National Park a few minutes from Mercer. Here we were able to see some incredible things in nature that have been in a transformation for tens of thousands of years. Erosion of creek beds helped show us some different soil layers, as well as seeing some original Native American pieces. The most interesting thing I found on this trip was the hut where the floor was carbon dated to over ten thousand years old! It's pretty amazing to see something that old, even if it's just something general like a floor. I have posted a picture of the entrance to the Indian Mound hut. It was also interesting to learn that these mounds were not ultimately found until fairly recently. The way they were actually discovered was human bones were sticking out.
Sunday, October 2, 2011
Blood Sugar
Blood sugar and the insulin response are a negative feedback loop, which means that it wants to resist change as much as possible. This loop wants to keep the body in homeostasis and when there are dips or spikes in blood sugar, return it back to normal levels. The hypothalamus has neurons that are used to detect glucose, and when your blood sugar spikes, insulin is produced. Insulin then changes the glucose into glycogen which decreases your blood sugar level. Insulin production is then stopped once this is complete, which is the negative feedback loop aspect.
Soil Lab
In this lab, we visited community gardens. This is basically a garden that many people contribute to and can utilize the products of the garden. These gardens are fairly new, only 30-50 years ago there were houses that rested on the same property where these gardens are now. That being said, the levels of lead in the soil are potentially concerning.
The way we deciphered what type of soil it was, was by using a soil dichotomous key. We used sieves to sift through the soil, where finer particles such as clay would fall through the sieve and thicker particles would stay on top.
The way we deciphered what type of soil it was, was by using a soil dichotomous key. We used sieves to sift through the soil, where finer particles such as clay would fall through the sieve and thicker particles would stay on top.
Soil Types
Soil Orders
Here is a link to the twelve different types of soil. One type that I found interesting was andisol, which is soil that is formed by volcanic ash. Globally this is the most rare type of soil, which accounts for around 1.7% of all the US soil. One trait of andisol soil is that it has a high-water holding capacity.
Andisol
Here is a link to the twelve different types of soil. One type that I found interesting was andisol, which is soil that is formed by volcanic ash. Globally this is the most rare type of soil, which accounts for around 1.7% of all the US soil. One trait of andisol soil is that it has a high-water holding capacity.
Andisol
This map shows the sub-orders of andisol soil and where they are prevalent. It's clear that andisol soil is seen almost exclusively in the Northwestern part of the United States.
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