[1] 马 敬.1994.磷胁迫下植物根系有机酸的分泌及其对土壤难溶性磷的活化[硕士学位论文].北京:北京农业大学.[2] 刘国栋、李继云、李振声.1995.植物高效利用磷营养的化学机理.植物营养与肥料学报, (3~4):72~78[3] 何振立、袁可能、朱祖祥.1990.有机阴离子对磷酸根吸附的影响.土壤学报,27(4):377~383.[4] Ae,N.,Arihara,J. and Okada,K. et al.1990. Phosphorus uptake by pigeon pea and its role in cropping system of the India subcontinent. Science, 248:477~480.[5] Ae,N.,Arihara,J.and Okada,K.1991.Phosphorus uptake mechanisms of pigeon pea grown in alfisols and vertisols. In: Phosphorus nutrient of grain legumes in the semi-arid tropics.Eds.Johansen,C.,Lee,K.K.and Sahrawat,K.L.pp.91~98. ICRISAT. Patancheru, India.[6] Bar-Yosef, B. 1991. Roots exertions and their environmental effects. Influence on availability of phosphorus. In: Plant Roots,the Hidden Half (Yoav Waisel,et al. eds.). Marcel Dekker,Inc. New York,Hong Kong, pp.529~557.[7] David, L. J. and Peter, R. D. 1994. Role of root derived organic acids in the mobilization of nutrients from the rhizosphere. Pland and Soil, 166:247~257.[8] Dinkelaker, B., Romheld,V. & Marschner,H. 1989. Citric acid excretion and precipitation of calcium citrate in the rhizosphere of white lupin (Lupinus albus L.).Plant,Cell and Environment,12:285~292.[9] Dinkelaker, B., Hengeler,C. & Marschner,H. 1995. Distribution and function of proteoid roots and other root clusters. Bot. Acta, 108:183~200.[10] Earl, K.D., Syers,J.K. and McLaughlin,J.R. 1979. Origin of the effects of citrate, tartrate,and acetate on phosphate sorption by soils and synthetic gels. Soil Sci.Am. J., 43:674~678.[11] Fox,T., Comerford,N.and McFee,W.1990a. Phosphorus and aluminum release from a spodic horizon mediated by organic acids. Soil Sci. Soc. Am.J., 54:1763~1767.[12] Fox,T., Comerford,N.and McFee,W. 1990b. Kinetics of phosphorus release from spodozols. Soil Sci. Soc. Am.J., 56:290~294.[13] Gardner,W. K., Parbery,D.G. and Barber, D.A. 1981. Proteoid root morphology and function in Lupinus albus L. Plant and Soil, 60:143~147.[14] Gardner,W. K., Parbery,D.G. and Barber, D.A. 1982. The acquisition of phosphorus by Lupinus albus L.Ⅱ. The effect of varying phosphorus supply and soil type on some characteristics of the soil/root interface. Plant and Soil, 68:33~41.[15] Gardner,W. K.,Barber, D.A. and Parbery,D.G. 1983 . The acquisition of phosphorus by Lupinus albus L. Ⅲ. The probable mechanism by which phosphorus movement in the soil/root interface is enhanced. Plant and Soil,70:107~124.[16] Gerke, J. 1993. Solubilizaion of Fe(Ⅲ) from humic-Fe complexes,humic/Fe-oxide mixtures and from poorly ordered Fe-oxide by organic acids-consequences for P adsorpion. Z.Pflanzenernahr,Bodenk., 156:253~257.[17] Gerke, J. 1994a. Kinetics of soil phosphate desorption as affected by citric acid. Z.Pflanzenernahr,Bodenk.,157:17~22.[18] Gerke, J., Wilhelm, R. and Albrecht, J. 1994b. The excretion of citric and malic acid by proteoid roots of Luinus albus L.; effect on soil solution concentions of phosphate,iron,and aluminum in the proteoid rhizophere in samples of an oxisol and a luvisol. Z.Pflanzenernahr,Bodenk., 157:289~294.[19] Hoffland, E.,Findenegg,G. R. and Nelmans, J. A. 1989a.Solubilization of rock phosphate by rape. I. Evaluation of the role of the nutrient uptake pattern. Plant and Soil, 113:155~160.[20] Hoffland, E.,Findenegg,G. R. and Nelmans, J. A. 1989b.Solubilization of rock phosphate by rape. II. Local root exudation of organic acids as a response to P-starvation. Plant and Soil, 113:161~165.[21] Indiati,R and Izza,C. 1981. Changes induced by some organic anions on phosphorus sorption isotherms and on released Fe and Al. Annali dell' Istituto Sperimentale per la Nutrizione delle Piante. 11:7~20.[22] Jane, F.J.,Carroll, P. V. and Deborah, L. A. 1996. Phosphorus deficiency in Lupinus albus. I.Altered lateral root development and enhanced expression of phosphoenolpyruvate carboxylase. Plant Physiol., 112:31~41.[23] Lewis,D.G. and Quirk,J.P. 1967. Phosphate diffusion in soils and uptake by plants. II. The phosphate uptake by wheat plants. Plant and Soil, 26:119~128.[24] Lipton,D.S.,Blanchar, R.W. and Blevins, D.G.1987. Citrate, malate and succinate concentration in exudation from P-sufficient and P-stressed Medicago sativa L. seedlings. Plant Physiol., 85: 315~317.[25] Marschner, H.,Romheld,V. and Cakmak, I. 1987. Root-induced changes of nutrient availability in the rhizosphere. J. Plant Nutr.,10:1175~1184.[26] Pohlman, A.A. and McColl, J.G.1986. Kinetics of metal dissolution from forest soils by soluble organic acids. J. Environ. Qual.,15:86~92.[27] Rosenfield, C. L., Reed, D. W. and Kent, M.W. 1991. Dependency of iron reduction on development of a unique root morphology in Ficus benjamina L. Plant Physiol.,95:1120~1124.[28] Strom, L., Olsson,T. and Tyler,G. 1994. Difference between calcifuge and acidifuge plants in root exudation of low-molecular organic acids. Plant and Soil, 67:239~245.[29] Tyler,G. and Strom, L.1995. Differing organic acid exudation pattern explains calcifuge and acidifuge behavior of plants. Annals of Botany,75:75~78. |