/AnMtgsAbsts2009.53780 Comparison of Intra-Aggregate Pore Characteristics From Soil in Conventional Row-Crop Agriculture and Native Succession Vegetation.

Monday, November 2, 2009
Convention Center, Exhibit Hall BC, Second Floor

Wei Wang1, Alexandra N. Kravchenko2, Kateryna Ananyeva1, Alvin J. M. Smucker2, Hyen Chung Chun3 and Mark L. Rivers4, (1)Michigan State Univ., East Lansing, MI
(2)Dept. of Crop and Soil Sciences, Michigan State Univ., East Lansing, MI
(3)Crop & Soil Sciences, Michigan State University, Lansing, MI
(4)CARS, Univ. of Chicago, Argonne, IL
Abstract:
Soil aggregates play an important role in many soil processes, including solution transport, storage of various nutrients and organic matters, and microbial activity. Past research indicates that microbial activities within soil matrix are highly spatially heterogeneous due to complex pore structure of soil aggregates. X-ray microtomography is a great tool that allows quantitatively describing and comparing aggregate structure and internal organization in aggregates from different soil types, agricultural practices and land uses.  In this study, we compared quantitative 3D pore/solid geometry of naturally air-dry aggregates from conventional row-crop agriculture (T1) and native successive vegetation (T7) from LTER main site, KBS, MI.The features we quantified includes several fluid flow related properties, i.e., burn number distribution, pore size distribution, throat area distribution, effective throat/pore radii ratio. Our preliminary results show that comparing to aggregates from T1, T7 aggregates  have significantly greater number of larger pores with pore networks in favor of fluid flow.