See more from this Session: Symposium--Mineral-Organic Interactions Across Time and Space: I & II
We investigated the response of soil C to silvicultural treatments (fertilization (F) and herbicide (H) and a cross (HF)) on similarly classified soils (parasesquic, mesic, Andic/Xeric Haplohumults) formed on two parent material ‘end members’ in this belt (silica rich quartzite (Q) vs intermediate to mafic volcanic mudflows (MF)). Analysis with X-ray diffraction indicates that site Q has abundant crystalline gibbsite and kaolinite with limited SRO materials while site MF possessed abundant SRO and kaolinite. Treatment affects on bulk soil C were not consistent across sites with increased C storage in surface soils at MF for F and HF (vs Control) and reduced C storage for H. There was little increase (F) to reduction (H and HF) of soil C at site Q. Differences are attributed to the capacity of SRO materials to store a portion of enhanced litter inputs related to fertilization while the more crystalline oxides at site Q could not capture these increases. This talk will report on the partitioning of C into organo-metallic complexes and associated with poorly and high crystalline iron and aluminum oxides extracted or remaining after selective dissolution analysis. Better understanding of site-treatment interactions based on soil oxide content could have interesting implications to soil C dynamics in managed forest ecosystem in California and around the world.
See more from this Session: Symposium--Mineral-Organic Interactions Across Time and Space: I & II