PHOSPHORUS-CONTENT IN THE SOIL MICROBIAL BIOMASS UNDER BRACHIARIA-DECUMBENS STAPF

Citation
Jgm. Guerra et al., PHOSPHORUS-CONTENT IN THE SOIL MICROBIAL BIOMASS UNDER BRACHIARIA-DECUMBENS STAPF, Pesquisa agropecuaria brasileira, 30(4), 1995, pp. 543-551
Citations number
NO
Categorie Soggetti
Agriculture,"Agriculture Dairy & AnumalScience
ISSN journal
0100204X
Volume
30
Issue
4
Year of publication
1995
Pages
543 - 551
Database
ISI
SICI code
0100-204X(1995)30:4<543:PITSMB>2.0.ZU;2-C
Abstract
Following a long-term experiment on the growth of Brachiaria decumbens fertilized with different sources of phosphorus applied at different times, a study was performed to estimate the phosphorus in the microbi al biomass using the fumigation-extraction method. The treatments were : no P fertilization (PO), rock phosphate incorporated 60 days before planting (RFpl), rock phosphate 60 days before planting and triple sup erphosphate applied 3 years later (RFpl + STcob), superphosphate at pl anting (STpl), superphosphate at full leaf cover (STcob), and superpho sphate at planting and 3 years later (STpl + STcob). The addition rate at each of the two stages of fertilizer application was equivalent to 87 kg P/ha. The microbial P increased from 7.7 to 13.7 mg P/kg soil w hen the soil was fertilized with superphosphate, either at planting, o r three years later at full leaf cover, resulting in an increase in th e P concentration in the biomass from 10.6 to 21.2 g P/kg biomass in t he same treatments. There was a tendency for the application of superp hosphate to cause a decrease in the C:P ratio of the biomass independe nt of the date of application. Thus, the plots fertilized with superph osphate at planting and again 3 years later, did not result in any inc rease in the P content in the microbial biomass when compared with the plots fertilized only at planting, showing that even after 5 years of growth of Brachiaria the soil microbial biomass was found to be highe r in P than in the treatment where there was no P fertilization. The m icrobial P was shown to be a promising parameter for studies of the fa te and dynamics of P in the soil.