Phosphorus characteristics correlate with soil fertility of albic luvisols
The information on phosphorus (P) characteristics of albic luvisols and their effect on plant P uptake is limited. Twelve soils representing typical albic luvisols were collected from farmland of four regions in northeast China, each with various levels of soil fertility. Phosphorus fractions, P ads...
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Published in: | Plant and soil Vol. 270; no. 1-2; pp. 47 - 56 |
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01-03-2005
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Abstract | The information on phosphorus (P) characteristics of albic luvisols and their effect on plant P uptake is limited. Twelve soils representing typical albic luvisols were collected from farmland of four regions in northeast China, each with various levels of soil fertility. Phosphorus fractions, P adsorption and P supply capacity of the soils were analysed and were correlated with soil fertility and plant P nutrition. Total P in these soils ranged from 0.62–0.91 g kg-1, and comprised 37–51% organic P, and 49–63% in inorganic forms among which the percentage of occluded P was the greatest, followed by Fe-P, Ca-P, Al-P and loosely bound P was the lowest (<1%). Whereas the % of organic P was not clearly affected by fertility, the % of occluded P increased with fertility. By contrast, both % and contents of other P forms decreased with decreasing soil fertility. Soil P adsorption maxima calculated from Langmuir isotherm ranged from 484 to 912 mg kg-1. Soils with low fertility had the strongest P adsorption, and those with medium fertility had the weakest in all collection regions. The supply capacity of P was positively related to soil fertility. Plant growth correlated positively with P forms with available P correlating best, followed by Fe-P and P supply capacity. Organic C correlated with available P, Fe-P, total P, Al-P and P supply capacity but not with organic P. The results suggest that though the albic luvisols contained high total P, they had low P availability, and P application is required for optimal crop production on these soils. |
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AbstractList | The information on phosphorus (P) characteristics of albic luvisols and their effect on plant P uptake is limited. Twelve soils representing typical albic luvisols were collected from farmland of four regions in northeast China, each with various levels of soil fertility. Phosphorus fractions, P adsorption and P supply capacity of the soils were analysed and were correlated with soil fertility and plant P nutrition. Total P in these soils ranged from 0.62--0.91 g kg--1, and comprised 37--51% organic P, and 49--63% in inorganic forms among which the percentage of occluded P was the greatest, followed by Fe-P, Ca-P, Al-P and loosely bound P was the lowest (<1%). whereas='' the='' %='' of='' organic='' p='' was='' not='' clearly='' affected='' by='' fertility,='' the='' %='' of='' occluded='' p='' increased='' with='' fertility.='' by='' contrast,='' both='' %='' and='' contents='' of='' other='' p='' forms='' decreased='' with='' decreasing='' soil='' fertility.='' soil='' p='' adsorption='' maxima='' calculated='' from='' langmuir='' isotherm='' ranged='' from='' 484='' to='' 912 mg=''>--1. Soils with low fertility had the strongest P adsorption, and those with medium fertility had the weakest in all collection regions. The supply capacity of P was positively related to soil fertility. Plant growth correlated positively with P forms with available P correlating best, followed by Fe-P and P supply capacity. Organic C correlated with available P, Fe-P, total P, Al-P and P supply capacity but not with organic P. The results suggest that though the albic luvisols contained high total P, they had low P availability, and P application is required for optimal crop production on these soils. The information on phosphorus (P) characteristics of albic luvisols and their effect on plant P uptake is limited. Twelve soils representing typical albic luvisols were collected from farmland of four regions in northeast China, each with various levels of soil fertility. Phosphorus fractions, P adsorption and P supply capacity of the soils were analysed and were correlated with soil fertility and plant P nutrition. Total P in these soils ranged from 0.62–0.91 g kg-1, and comprised 37–51% organic P, and 49–63% in inorganic forms among which the percentage of occluded P was the greatest, followed by Fe-P, Ca-P, Al-P and loosely bound P was the lowest (<1%). Whereas the % of organic P was not clearly affected by fertility, the % of occluded P increased with fertility. By contrast, both % and contents of other P forms decreased with decreasing soil fertility. Soil P adsorption maxima calculated from Langmuir isotherm ranged from 484 to 912 mg kg-1. Soils with low fertility had the strongest P adsorption, and those with medium fertility had the weakest in all collection regions. The supply capacity of P was positively related to soil fertility. Plant growth correlated positively with P forms with available P correlating best, followed by Fe-P and P supply capacity. Organic C correlated with available P, Fe-P, total P, Al-P and P supply capacity but not with organic P. The results suggest that though the albic luvisols contained high total P, they had low P availability, and P application is required for optimal crop production on these soils. The information on phosphorus (P) characteristics of albic luvisols and their effect on plant P uptake is limited. Twelve soils representing typical albic luvisols were collected from farmland of four regions in northeast China, each with various levels of soil fertility. Phosphorus fractions, P adsorption and P supply capacity of the soils were analysed and were correlated with soil fertility and plant P nutrition. Total P in these soils ranged from 0.62-0.91 g kg^sup -1^, and comprised 37-51% organic P, and 49-63% in inorganic forms among which the percentage of occluded P was the greatest, followed by Fe-P, Ca-P, Al-P and loosely bound P was the lowest (<1%). Whereas the % of organic P was not clearly affected by fertility, the % of occluded P increased with fertility. By contrast, both % and contents of other P forms decreased with decreasing soil fertility. Soil P adsorption maxima calculated from Langmuir isotherm ranged from 484 to 912 mg kg^sup -1^. Soils with low fertility had the strongest P adsorption, and those with medium fertility had the weakest in all collection regions. The supply capacity of P was positively related to soil fertility. Plant growth correlated positively with P forms with available P correlating best, followed by Fe-P and P supply capacity. Organic C correlated with available P, Fe-P, total P, Al-P and P supply capacity but not with organic P. The results suggest that though the albic luvisols contained high total P, they had low P availability, and P application is required for optimal crop production on these soils.[PUBLICATION ABSTRACT] |
Author | Han, X.Z Qiao, Y.F Song, C.Y Tang, C Wang, S.Y |
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Cites_doi | 10.1097/00010694-197604000-00003 10.1097/01.ss.0000106408.84926.8f 10.1111/j.1365-2389.1983.tb01069.x 10.1016/j.fcr.2003.08.013 10.2134/jeq2004.0965 10.1097/00010694-195708000-00005 10.1111/j.1475-2743.2000.tb00194.x 10.2136/sssaj1957.03615995002100020004x 10.1097/00010694-199206000-00004 10.1111/j.1365-2389.1966.tb01452.x 10.1097/00010694-195010000-00002 10.2136/sssaj1970.03615995003400060025x 10.2136/sssabookser3.3ed 10.1021/es00006a020 10.1007/BF00750096 |
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Keywords | Fractionation Soil fertility phosphorus release Property of soil Soil quality Phosphorus Agricultural soil Inorganic element Langmuir isotherm phosphorus fractionation Adsorption Luvisols Characteristics phosphorus adsorption Soil plant relation Release |
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References_xml | – volume: 121 start-page: 205 year: 1976 ident: 1083_CR5 publication-title: Soil Sci. doi: 10.1097/00010694-197604000-00003 contributor: fullname: R L Evans – volume: 168 start-page: 869 year: 2003 ident: 1083_CR10 publication-title: Soil Sci. doi: 10.1097/01.ss.0000106408.84926.8f contributor: fullname: J C Hansen – volume: 34 start-page: 751 year: 1983 ident: 1083_CR1 publication-title: J. Soil Sci. doi: 10.1111/j.1365-2389.1983.tb01069.x contributor: fullname: N J Barrow – volume: 86 start-page: 225 year: 2004 ident: 1083_CR25 publication-title: Field Crop Res. doi: 10.1016/j.fcr.2003.08.013 contributor: fullname: J Shen – volume: 33 start-page: 965 year: 2004 ident: 1083_CR13 publication-title: J. Environ. Qual. doi: 10.2134/jeq2004.0965 contributor: fullname: G F Koopmans – volume: 84 start-page: 133 year: 1957 ident: 1083_CR3 publication-title: Soil Sci. doi: 10.1097/00010694-195708000-00005 contributor: fullname: S C Chang – volume: 16 start-page: 206 year: 2000 ident: 1083_CR12 publication-title: Soil Use Manage. doi: 10.1111/j.1475-2743.2000.tb00194.x contributor: fullname: S Hughes – volume-title: Methods for Agrochemical Analysis of Soils year: 1999 ident: 1083_CR16 contributor: fullname: R K Lu – volume: 21 start-page: 144 year: 1957 ident: 1083_CR19 publication-title: Soil Sci. Soc. Am. Proc. doi: 10.2136/sssaj1957.03615995002100020004x contributor: fullname: S R Olsen – volume-title: FAO-UNESCO Soil Map of the World, Revised Legend. World Soil resources report 60 year: 1988 ident: 1083_CR6 contributor: fullname: FAO – volume-title: Estimation of Available Phosphorus in Soils by Extraction with Sodium Bicarbonate year: 1954 ident: 1083_CR20 contributor: fullname: S R Olsen – start-page: 869 volume-title: Methods of Soil Analysis, Part 3 – Chemical Analysis year: 1996 ident: 1083_CR14 contributor: fullname: S Kuo – start-page: 141 volume-title: Soil Testing and Plant Analysis year: 1990 ident: 1083_CR7 contributor: fullname: P E Fixen – volume-title: Australian Laboratory Handbook of Soil and Water Chemical Methods year: 1992 ident: 1083_CR22 contributor: fullname: G E Rayment – volume-title: Methods of Soil Analysis. Part 2. Chemical and microbiological properties year: 1965 ident: 1083_CR2 contributor: fullname: C A Black – volume: 153 start-page: 452 year: 1992 ident: 1083_CR21 publication-title: Soil Sci. doi: 10.1097/00010694-199206000-00004 contributor: fullname: H B Pionke – volume: 17 start-page: 56 year: 1966 ident: 1083_CR4 publication-title: J. Soil Sci. doi: 10.1111/j.1365-2389.1966.tb01452.x contributor: fullname: I J Cooke – volume: 70 start-page: 257 year: 1950 ident: 1083_CR11 publication-title: Soil Sci. doi: 10.1097/00010694-195010000-00002 contributor: fullname: J F Hasemen – start-page: D18 volume-title: Handbook of Soil Science year: 2000 ident: 1083_CR24 contributor: fullname: A Sharpley – volume: 34 start-page: 902 year: 1970 ident: 1083_CR8 publication-title: Soil Sci. Soc. Am. Proc. doi: 10.2136/sssaj1970.03615995003400060025x contributor: fullname: R L Fox – volume-title: Handbook of Agricultural Chemistry year: 1982 ident: 1083_CR17 contributor: fullname: R K Lu – volume: 29 start-page: 13 year: 1997 ident: 1083_CR9 publication-title: China Soil Sci. contributor: fullname: Y C Gu – volume-title: Soil testing and plant analysis year: 1990 ident: 1083_CR26 doi: 10.2136/sssabookser3.3ed contributor: fullname: R L Westerman – volume: 29 start-page: 1569 year: 1995 ident: 1083_CR15 publication-title: Environ. Sci. Technol. doi: 10.1021/es00006a020 contributor: fullname: R Lookman – volume: 40 start-page: 121 year: 1995 ident: 1083_CR23 publication-title: Fertilizer Res. doi: 10.1007/BF00750096 contributor: fullname: K N Sharma – start-page: 187 volume-title: Soil Analysis – An Interpretation Manual year: 1999 ident: 1083_CR18 contributor: fullname: P W Moody |
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Snippet | The information on phosphorus (P) characteristics of albic luvisols and their effect on plant P uptake is limited. Twelve soils representing typical albic... |
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SubjectTerms | Acid soils Adsorption Agricultural land Agricultural soils Agrology Agronomy. Soil science and plant productions bioassays Biological and medical sciences Clay soils corn Crop production Fertility Fundamental and applied biological sciences. Psychology General agronomy. Plant production nutrient availability Organic soils Phosphorus Plant growth Plant nutrition Sedimentary soils Soil fertility soil nutrients Soil organic matter Soil science soil-plant interactions Soil-plant relationships. Soil fertility Soil-plant relationships. Soil fertility. Fertilization. Amendments Soils Zea mays |
Title | Phosphorus characteristics correlate with soil fertility of albic luvisols |
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