Understanding how the concentration and chemical quality of dissolved organic matter
(DOM) varies in soils is critical because DOM influences an array of biological, chemical …

Soil bulk density (ρb) is required to estimate, evaluate, and calculate many physical soil
properties and processes and is essential to convert data from weight‐based to volume‐and …

Aquatic Dicotyledons of North America: Ecology, Life History, and Systematics brings
together a wealth of information on the natural history, ecology, and systematics of North …

Accurate soil organic carbon (SOC) maps are needed to predict the terrestrial SOC feedback
to climate change, one of the largest remaining uncertainties in Earth system modeling. Over …

Abstract The Tongass National Forest (Tongass) is the largest national forest and largest
area of old-growth forest in the United States. Spatial geographic information system data for …

High‐latitude warming could cause northern peatlands to become C sources. Where
peatlands border boreal forests, strong differences in ecosystem C balances reflect drainage …

Understanding the sources and removal mechanisms for dissolved organic matter (DOM) in
soils is critical to determining the importance of peatlands in influencing streamwater DOM …

To improve our ability to predict how different wetland soils cycle nutrients, it is necessary to
gain an understanding of N and P net mineralization rates. Since information on …

Small changes in C cycling in boreal forests can change the sign of their C balance, so it is
important to gain an understanding of the factors controlling small exports like water-soluble …

Highland environments favor accumulation and preservation of soil organic matter (SOM)
due to low temperatures, leading to the formation of Histosols. The Itatiaia National Park …