The relative contribution of plant residues and fertilizer to the phosphorus nutrition of wheat in a pasture cereal system

Soil Research ◽  
1986 ◽  
Vol 24 (4) ◽  
pp. 517 ◽  
Author(s):  
MJ Mclaughlin ◽  
AM Alston

Wheat plants (Triticum aestivum cv. Warigal) here grown in a solonised brown soil (Calcixerollic xerochrept) which had been previously cropped to medic (Medicago trunculata cv. Paraggio). The 33P-labelled medic residues and 32P-labelled monocalcium phosphate were added to the soil in factorial combination. Amounts of 31P, 32P and 33P in the wheat plants and in the soil microbial biomass were determined. Addition of residues depressed wheat dry weight, 31P and 32P uptake, while simultaneously increasing amounts of 31P and 32P incorporated into the microbial biomass. Addition of fertiliser had no effect on the proportion of plant P taken up from the residues, but significantly increased the proportion of microbial P derived from this source. The 31P held in the microbial biomass was significantly increased by both residue and fertiliser P addition, with the former having the larger effect. Of the total P applied to the soil, medic residues contributed approximately one-quarter of that supplied by the fertiliser. Of the total P in the wheat plant, medic residues supplied approximately one-fifth of that supplied by the fertiliser.

Author(s):  
K.W. Perrott ◽  
S.U. Sarathchandra

Significant quantities of phosphorus (P) and nitrogen (N) are present in the soil microbes compared with pasture requirements for these nutrients. Seasonal and fertiliser effects on microbial P and N were investigated in a controlled environment (CE) experiment, two field trials and a glasshouse trial. In the CE experiment there was a basic seasonal pattern of storage of P and N by the microbial biomass over "winter" and release of these nutrients in "spring". Climatic variations affected this pattern in the field trials. Withholding fertiliser did not affect soil microbial P and N in the field trials, despite a decline in pasture production of up to 20%. Soil microbial P and N did decline in the glasshouse trial, in which a much larger drop in herbage production (X30%) was induced by nutrient deficiency. Keywords soil microbial biomass, microbial phosphorus, microbial nitrogen, seasonal effects, withholding fertiliser, plant nutrients


1998 ◽  
Vol 17 (8) ◽  
pp. 1462-1468 ◽  
Author(s):  
Andrew A. Meharg ◽  
Clare L. Wyatt ◽  
Ian P. Thompson ◽  
Mark J. Bailey ◽  
Richard J. Ellis ◽  
...  

Soil Research ◽  
1988 ◽  
Vol 26 (2) ◽  
pp. 333 ◽  
Author(s):  
MJ Mclaughlin ◽  
AM Alston ◽  
JK Martin

The incorporation of phosphorus derived from fertilizer and plant residues into the soil microbial biomass was studied under field conditions by using isotopic double labelling. The 33P-labelled medic residues (Medicago truncatula cv. Paraggio) and 32P-labelled fertilizer were added to a solonized brown soil (Calcixerollic xerochrept) before sowing of a wheat crop ( Triticum aestivum cv. Warigal). Amounts of 31P, 32P and 33P in the microbial biomass were determined at 0, 7, 18, 32, 46, 61, 81 and 95 days after sowing of the wheat. Throughout the experiment, amounts of 31P in the microbial biomass were closely related to gravimetric soil water content, with a large and rapid increase in the amount of 3 1 ~ in the microbial biomass being observed in the first 7 days after wetting of the (initially) dry soil. Due to banding of the fertilizer at sowing, little (<5%) of the 32P was recovered in the microbial biomass throughout the experiment. Of the 33P applied in the medic residues, 22-28% was recovered in the microbial biomass. Most of the P taken up by the microbial biomass was derived from native soil P (i.e. not added that season).


2003 ◽  
Vol 38 (8) ◽  
pp. 955-962 ◽  
Author(s):  
Gabriela Bielefeld Nardoto ◽  
Mercedes Maria da Cunha Bustamante

The objective of this work was to study the effects of fire on net N mineralization and soil microbial biomass in burned and unburned cerrado stricto sensu sites. The study was carried out from April 1998 to April 2000. The pH values were significantly higher in the burned site while soil moisture content was significantly higher in the unburned site (P<0.05). The soil C/N ratio was 22/1 and the available NO3-N ranged between 1.5 and 2.8 mg kg-¹ dry weight. However, the NH4-N concentration ranged between 3 and 34 mg kg-1 dry weight in the burned site and between 3 and 22 mg kg-1 dry weight in the unburned site. The NH4-N increased after fire, but no significant changes were observed for NO3-N (P<0.05). The NO3-N accumulation occurred in short periods during the rainy season. The rates of net N mineralization increased during the rainy season while reductions in soil microbial biomass were observed at both sites. This suggested that the peak in microbial activities occurred with the first rain events, with an initial net immobilization followed by net mineralization. Both sites presented the same pattern for mineralization/immobilization, however, the amount of inorganic-N cycled annually in unburned site was 14.7 kg ha-1 per year while the burned site presented only 3.8 kg ha-¹ of inorganic-N, one year after the burning.


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