Abstract: Soil mixing and transport increase inventories of mineral surface area and organic carbon, with systematic shifts in C/N, δ<sup>13</sup>C, and δ<sup>15</sup>N, along a forested hillslope transect (2017 AGU Fall Meeting)

Soil mixing and transport increase inventories of mineral surface area and organic carbon, with systematic shifts in C/N, δ¹³C, and δ¹⁵N, along a forested hillslope transect

Beth Fisher, University of Minnesota Twin Cities, Minneapolis, MN, United States, Kyungsoo Yoo, Univ of MN-Soil, Water&Climate, St. Paul, MN, United States, Anthony Keith Aufdenkampe, LimnoTech, Central Region Office, Ann Arbor, MI, United States, Edward A Nater, Univ of MN /Soil Water&Climate, St. Paul, United States, Rolf E Aalto, University of Exeter, Geography, Exeter, EX4, United Kingdom and Julia Marquard, University of Exeter, Geography, Exeter, United Kingdom

Back to: Soil Organic Matter and the Global Carbon Cycle: Mechanisms for Accumulation and Loss in a Changing World III

Soil mixing and transport increase inventories of mineral surface area and organic carbon, with systematic shifts in C/N, δ13C, and δ15N, along a forested hillslope transect

Soil mixing and transport increase inventories of mineral surface area and organic carbon, with systematic shifts in C/N, δ¹³C, and δ¹⁵N, along a forested hillslope transect