Characteristics of phosphate rock materials from China, Indonesia and Tunisia and their dissolution in Indonesian acid soils

Dissolution of phosphate rock (PR) in soils is a primary concern for P in the PR to be available for plant. The dissolution of three PR materials, China (CPR), Ciamis (IPR) and Gafsa (GPR), in eight acid Indonesian soils (pH in water 4.1-5.7) was tested in a closed incubation system. Experiment was...

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Main Authors: Hilman, Yusdar, Musa, Mohamed Hanafi, Abdul Rahim, Anuar, Hashim, Azizah, Adiningsih, Justina Sri
Format: Article
Language:English
Published: Indonesian Agency for Agriculture Research and Development 2006
Online Access:http://psasir.upm.edu.my/id/eprint/52428/1/Characteristics%20of%20phosphate%20rock%20materials%20from%20China%2C%20Indonesia%20and%20Tunisia%20and%20their%20dissolution%20in%20Indonesian%20acid%20soils.pdf
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author Hilman, Yusdar
Musa, Mohamed Hanafi
Abdul Rahim, Anuar
Hashim, Azizah
Adiningsih, Justina Sri
author_facet Hilman, Yusdar
Musa, Mohamed Hanafi
Abdul Rahim, Anuar
Hashim, Azizah
Adiningsih, Justina Sri
author_sort Hilman, Yusdar
collection UPM
description Dissolution of phosphate rock (PR) in soils is a primary concern for P in the PR to be available for plant. The dissolution of three PR materials, China (CPR), Ciamis (IPR) and Gafsa (GPR), in eight acid Indonesian soils (pH in water 4.1-5.7) was tested in a closed incubation system. Experiment was conducted in Soil Chemical Laboratory, Universiti Putra Malaysia and Indonesian Center for Agricultural Land Resources Research and Development from January to April 2002. The dissolution was determined from the increase in either 0.5 M NaOH extractable P (∆P) or 1 M BaCl2-triethanolamine (TEA)-extractable Ca (∆Ca) in soils amended with PR compared with control soil. Dissolution of the IPR was the highest (30-100%) followed by GPR (17-69%) and then by CPR (20-54%). The maximum dissolution followed the order: Bogor Ultisols > Bogor Oxisols > Subang Inceptisols > Bogor Inceptisols > Sukabumi Oxisols > Lebak Ultisols > Sukabumi Inceptisols > Lampung Ultisols. PR dissolution indicated a positive correlation with P retention capacity. The results implied that the extent of PR dissolution for the three PR sources (China, Indonesia and Tunisia) increased with increasing P retention capacity of the soils. PR dissolution can be based on a calibration curve of ∆Ca meaning that if ∆P is high then the amount of PR dissolution measured by ∆Ca in PR materials is also high.
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spelling upm.eprints-524282017-06-06T08:43:22Z http://psasir.upm.edu.my/id/eprint/52428/ Characteristics of phosphate rock materials from China, Indonesia and Tunisia and their dissolution in Indonesian acid soils Hilman, Yusdar Musa, Mohamed Hanafi Abdul Rahim, Anuar Hashim, Azizah Adiningsih, Justina Sri Dissolution of phosphate rock (PR) in soils is a primary concern for P in the PR to be available for plant. The dissolution of three PR materials, China (CPR), Ciamis (IPR) and Gafsa (GPR), in eight acid Indonesian soils (pH in water 4.1-5.7) was tested in a closed incubation system. Experiment was conducted in Soil Chemical Laboratory, Universiti Putra Malaysia and Indonesian Center for Agricultural Land Resources Research and Development from January to April 2002. The dissolution was determined from the increase in either 0.5 M NaOH extractable P (∆P) or 1 M BaCl2-triethanolamine (TEA)-extractable Ca (∆Ca) in soils amended with PR compared with control soil. Dissolution of the IPR was the highest (30-100%) followed by GPR (17-69%) and then by CPR (20-54%). The maximum dissolution followed the order: Bogor Ultisols > Bogor Oxisols > Subang Inceptisols > Bogor Inceptisols > Sukabumi Oxisols > Lebak Ultisols > Sukabumi Inceptisols > Lampung Ultisols. PR dissolution indicated a positive correlation with P retention capacity. The results implied that the extent of PR dissolution for the three PR sources (China, Indonesia and Tunisia) increased with increasing P retention capacity of the soils. PR dissolution can be based on a calibration curve of ∆Ca meaning that if ∆P is high then the amount of PR dissolution measured by ∆Ca in PR materials is also high. Indonesian Agency for Agriculture Research and Development 2006 Article PeerReviewed application/pdf en http://psasir.upm.edu.my/id/eprint/52428/1/Characteristics%20of%20phosphate%20rock%20materials%20from%20China%2C%20Indonesia%20and%20Tunisia%20and%20their%20dissolution%20in%20Indonesian%20acid%20soils.pdf Hilman, Yusdar and Musa, Mohamed Hanafi and Abdul Rahim, Anuar and Hashim, Azizah and Adiningsih, Justina Sri (2006) Characteristics of phosphate rock materials from China, Indonesia and Tunisia and their dissolution in Indonesian acid soils. Indonesian Journal of Agricultural Science, 7 (2). pp. 43-50. ISSN 1411-982X; ESSN: 2354-8509 http://ejurnal.litbang.pertanian.go.id/index.php/ijas/article/view/632
spellingShingle Hilman, Yusdar
Musa, Mohamed Hanafi
Abdul Rahim, Anuar
Hashim, Azizah
Adiningsih, Justina Sri
Characteristics of phosphate rock materials from China, Indonesia and Tunisia and their dissolution in Indonesian acid soils
title Characteristics of phosphate rock materials from China, Indonesia and Tunisia and their dissolution in Indonesian acid soils
title_full Characteristics of phosphate rock materials from China, Indonesia and Tunisia and their dissolution in Indonesian acid soils
title_fullStr Characteristics of phosphate rock materials from China, Indonesia and Tunisia and their dissolution in Indonesian acid soils
title_full_unstemmed Characteristics of phosphate rock materials from China, Indonesia and Tunisia and their dissolution in Indonesian acid soils
title_short Characteristics of phosphate rock materials from China, Indonesia and Tunisia and their dissolution in Indonesian acid soils
title_sort characteristics of phosphate rock materials from china indonesia and tunisia and their dissolution in indonesian acid soils
url http://psasir.upm.edu.my/id/eprint/52428/1/Characteristics%20of%20phosphate%20rock%20materials%20from%20China%2C%20Indonesia%20and%20Tunisia%20and%20their%20dissolution%20in%20Indonesian%20acid%20soils.pdf
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