Soil carbon "sequestration" is all the rage now a days, but very rarely does anyone define the time-frame of "sequester". Usually folks are only looking at changes to soil carbon *content*, and assuming those changes are permanent. They are not. Here we show that soil carbon *content* is de-coupled from how long that soil carbon stays in soil (i.e. having more carbon in soils does not necessary mean that carbon sticks around for longer periods of time).
Too many people focus on surface soils, and too many people ignore Manganese (Mn)! If you don't know about Mn's role in ecosystems processes, the introduction is expertly written by Dr. Angela Possinger (also the primary author) and is worth reading over. We show that Mn abundance at the continental scale is highly variable, but that it can be predictive of certain soil carbon metrics (especially lignin abundance). But, the effects of Mn is pretty unique on location, and at each horizon in the soil illustrating the old addage "it's all about site specificity!"
Permafrost soils are some of the coolest things I've ever seen, and the primary author, Dr. Erin Rooney, is showing us all her chemistry skills from the second chapter of her dissertation. If you want to see her first chapter, see her other permafrost paper above that describes some of the *physical* changes to permafrost when it undergoes freeze thaw cycles. But this paper is about the *chemical* changes that occur, and what that could mean for arctic-permafrost nutrient cycling.
Permafrost soils are finally getting the attention they deserve. Unfortunately, they may not be around much longer because of how quickly they are thawing. Here we explore what happens during freeze-thaw cycles that may alter their future behavior
Too many people focus on surface soils, and they're missing out on most of the (soil carbon) action when they do. Here we show that ecosystems favoring forests (wetter, more iron and aluminum) release more CO2 compared to grassland-like ecosystems (dryer, more calcium and magnesium). As our earth warms, we need to consider not only how surface soils will change due to management, but how subsurface soils (where most of the carbon is) will respond due to climate change.
SOM *storage* is not the same as its *vulnerability*. This was a 1-yr incubation experiment from NEON's A and B horizons ran by Tyler Weiglein at Virginia Tech as his Masters degree. We found that predictors of soil carbon vulnerability (based on CO2 respiration) were different for surface and subsurface horizons. Turns out, you need to dig deeper to find out the whole story on soils.
Chicken or the egg. Grassland soil carbon behaves different than forest soil carbon. But is that because of the plant composition? (No). Or is it because of the climatic differences? (Probably) But if the climatic differences *also* lead to vegetation differences, then how can you separate out the climate from the vegetation? Here we attempt to do so.
Although the field of soil science is _literally_ studying the land we live on, very rarely do we ask how this land came to be managed by the current people in power. In this paper we examine how America's past influences the current system of private and public land management agencies, and what we *must* do within the field of soil science to make a science for all people.
Studying wildfire effects on ecosystems is difficult because predicting *where* and *when* something will burn is nearly impossible, and rarely do you have robust pre-fire data. My dissertation samples from the Great Smoky Mountain National Park were collected prior to the Chimney Tops 2 from 2016. It was a wind-driven high intensity and high severity fire that burned 4,500 hectares. In this paper, we examine the pre and post fire pyrogenic carbon signal using an innovative BPCA method developed by Dr. Matosziuk.