Lj. Sikora et V. Yakovchenko, SOIL ORGANIC-MATTER MINERALIZATION AFTER COMPOST AMENDMENT, Soil Science Society of America journal, 60(5), 1996, pp. 1401-1404
The addition of composts and manures to soils has often resulted in in
creased plant yields that are not obviously related to the nutrients i
n the added organic material. A study was conducted to determine if co
mpost additions to soil resulted in increased mineralization of soil o
rganic matter (SOM). The organic matter of a Sassafras sandy loam soil
(fine-loamy, siliceous, mesic Typic Hapludult) was labeled with C-14
by incubating uniformly labeled wheat (Triticum aestivum L.) straw wit
h the soil through a minimum of 60 wetting-drying cycles during 2 yr.
A municipal solid waste-biosolids compost (MSWC) or a biosolids compos
t (BC) was added to the labeled soil or to acid-washed sand and incuba
ted for 1440 h. Decomposition of MSWC was low with 95% of the compost-
C remaining in sand or soil after 1440 h. Ninety-two percent of BC-C r
emained in sand and 86% remained in soil after 1440 h. Total and (CO2)
-C-14 data indicated that neither compost stimulated SOM decomposition
. Municipal solid waste-biosolids compost reduced slightly SOM decompo
sition at 545 and 715 h, The soil, however, stimulated BC decompositio
n. Nitrogen mineralization of the BC + soil mixture was greater than s
oil alone, and the N apparently came from the compost. The benefits fr
om addition of BC to Sassafras soil was not attributed to increased mi
neralization of SOM.