Behaviour of plant-derived extracellular phytase upon addition to soil

被引:102
作者
George, TS [1 ]
Richardson, AE [1 ]
Simpson, RJ [1 ]
机构
[1] CSIRO, Planat Ind, Canberra, ACT 2601, Australia
关键词
alfisol; Arabidopsis thaliana; enzyme adsorption; organic phosphorus; oxisol; pH; phosphatase; phytate; rhizosphere; spodosol;
D O I
10.1016/j.soilbio.2004.10.016
中图分类号
S15 [土壤学];
学科分类号
0903 ; 090301 ;
摘要
The behaviour of phytase after addition to three soil types with different sorption capacities was investigated. Phytase was collected from the roots of transgenic Arabidopsis thaliana that express a phytase gene from Aspergillus niger. Phytase activity in solution and on the solid phase of the soil was monitored over time. Phytase added to the solution phase of a soil suspension (1:20, w/v) was almost completely lost within 10 min in all soil types, while phytase in non-soil controls remained active in solution. Phytase activity lost from solution was recovered on the soil solid phase, suggesting rapid adsorption of the enzyme. Adsorption of phytase was less in soil taken from the rhizosphere of transgenic plants expressing phyA, indicating that the rhizosphere environment may help maintain phytase activity in solution. The activity of adsorbed phytase declined with time at a rate 2-4 times slower than that in the absence of soil. Adsorption of phytase in soils was highest at pH 4.5, which is below the reported isoelectric point (pI) of the Aspergillus phytase. As soil pH increased, adsorption decreased until, at pH 7.5, all phytase was in solution. Where phytase remained in solution, activity was maintained for at least 8 d. In contrast, the activity of adsorbed phytase was increasingly inhibited with time, particularly at low pH. By increasing the pH in soil suspensions, phytase that had remained active on the soil solid phase for 28 d was almost totally desorbed. Rapid immobilisation of phytase in soil may limit its capacity to interact with phytate, and this may compromise the ability of transgenic plants which exude phytase from their roots to acquire P from endogenous soil phytate. (c) 2004 Elsevier Ltd. All rights reserved.
引用
收藏
页码:977 / 988
页数:12
相关论文
共 52 条
[1]  
Anderson G., 1980, Khasawneh, F. E.
[2]  
Sample, E. C.
[3]  
Kamprath, E. J. : The role of phosphorus in agriculture. (Proceedings of a symposium held 1-3 June 1976 at the National Fertilizer Development Center, Tennessee Valley Authority, Muscle Shoals, Alabama)., P411
[4]   NATURE OF ALKALI-SOLUBLE SOIL ORGANIC PHOSPHATES [J].
ANDERSON, G ;
MALCOLM, RE .
JOURNAL OF SOIL SCIENCE, 1974, 25 (03) :282-297
[5]  
AVERY BW, 1974, SOIL SURVEY TECHNOLO, V6
[6]   CONCERNING LOCATION AND PERSISTENCE OF SOIL UREASE [J].
BURNS, RG ;
PUKITE, AH ;
MCLAREN, AD .
SOIL SCIENCE SOCIETY OF AMERICA PROCEEDINGS, 1972, 36 (02) :308-&
[7]   IMMOBILIZATION OF ALKALINE-PHOSPHATASE BY SORPTION ON NA-SEPIOLITE [J].
CARRASCO, MS ;
RAD, JC ;
GONZALEZCARCEDO, S .
BIORESOURCE TECHNOLOGY, 1995, 51 (2-3) :175-181
[8]  
COLWELL J. D., 1963, AUSTRALIAN JOUR EXPTL AGRIC AND ANIMAL HUSB, V3, P190, DOI 10.1071/EA9630190
[9]   KINETICS AND ACTIVITIES OF PHOSPHATASE-CLAY COMPLEXES [J].
DICK, WA ;
TABATABAI, MA .
SOIL SCIENCE, 1987, 143 (01) :5-15
[10]  
ESTERMANN EVA F., 1959, SOIL SCI SOC AMER PROC, V23, P31