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Effects of tillage and crop rotation on chemical phosphorus forms and some related biological activities in a Chilean Ultisol
Author(s) -
Redel Y. D.,
Escudey M.,
Alvear M.,
Conrad J.,
Borie F.
Publication year - 2011
Publication title -
soil use and management
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 0.709
H-Index - 81
eISSN - 1475-2743
pISSN - 0266-0032
DOI - 10.1111/j.1475-2743.2011.00334.x
Subject(s) - ultisol , tillage , phosphorus , chemistry , crop rotation , biomass (ecology) , crop , zoology , conventional tillage , agronomy , soil water , biology , ecology , organic chemistry
The effect of tillage systems and crop rotation on microbial biomass phosphorus (MBP) and acid phosphatase (P‐ase) activity, and the amount of different phosphorus (P) forms measured by 31 P‐NMR spectroscopy were studied on a field experiment carried out in a temperate Ultisol from southern Chile. Two tillage systems, no tillage (NT) and conventional tillage (CT) and two crop rotations, oat–wheat (OW) and lupine–wheat (LW) were evaluated 4 yr after the start of the experiment to determine the effects of such management on some soil biological parameters and P forms at three depths (0–5, 0–10 and 10–20 cm). Microbial biomass P ranged from 6.5 to 22.6 mg/kg, whereas the mean total P (P T ) was 1995 mg/kg for all treatments (OW and LW). Microbial biomass carbon (MBC) and surface P accumulation (at 0–5 cm depth), including Olsen P, MBP, orthophosphate monoesters (monoester‐P), were larger under NT than CT. Tillage effects were greater than crop rotation effects in enhancing P availability. The LW rotation showed enhanced P‐ase activity and increased monoester‐P forms (57 vs. 30% of the total integral area of the spectra, in average) compared with OW. Nevertheless, OW rotation increased orthophosphate (ortho‐P), especially at 10–20 cm. Microbial biomass carbon ranged from 532 to 2351 mg/kg, which represented 1.2–4.5% of total organic C (C o ). Furthermore, MBP correlated positively with MBC ( r = 0.80), Olsen P ( r = 0.77), C o ( r = 0.77), pH ( r = 0.65), P T ( r = 0.65) and P‐ase activity ( r = 0.57), suggesting the importance of the microbial biomass on soil P availability.