Characterization and Amelioration of Selected Acid Sulfate Soils in Malaysia

Researchers in the past had focused their study on the common or standard acid sulfate soils, which are characterized by high iron and the presence of jarosite mottles. Little is known about the characteristics and management of iron-poor acid sulfate soils and this study was conducted to provide...

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Main Author: Sarwani, Muhrizal
Format: Thesis
Language:English
English
Published: 2001
Subjects:
Online Access:http://psasir.upm.edu.my/id/eprint/10549/1/FP_2001_9.pdf
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author Sarwani, Muhrizal
author_facet Sarwani, Muhrizal
author_sort Sarwani, Muhrizal
collection UPM
description Researchers in the past had focused their study on the common or standard acid sulfate soils, which are characterized by high iron and the presence of jarosite mottles. Little is known about the characteristics and management of iron-poor acid sulfate soils and this study was conducted to provide the dearth of information. This study aimed to characterize and ameliorate acid sulfate soils in Malaysia. Three common acid sulfate soils in Malaysia namely Teluk, Jawa and Linau series were investigated in three phases. The first phase was concentrated on the characterization of the soils. The second phase dealt with laboratory incubation experiments to study oxidation processes. The third phase was on the ameliorative effects of organic materials, lime, phosphate and silicate application on acid sulfate soils. Results of the study revealed the presence of both iron-rich and iron-poor acid sulfate soils in Malaysia. The former, represented by the Teluk and Jawa soils, had thick accumulation of iron in the B-horizon. They followed the standard morphological profile commonly found under tropical monsoon climate. The latter, represented by the Linau soil, was low in iron content in the B-horizon. They followed the standard morphological profile commonly found under tropical monsoon climate. The latter, represented by the Linau soil, was low in iron content in the B-horizon. The low content of iron was most probably due to high organic content enhanced by wet climate in Malaysia. The formation of Fe (III) oxide was hindered when the environment was rich in organics. Incubation study indicated that oxidation of pyrite resulted in a decrease in pH and the formation of jarosite which, in tum, transformed into short-range order Fe-oxides. The yellow mottles formed during pyrite oxidation were jarosite/natrojarosite and alunite as detected by X-ray diffraction analysis. The oxidation of pyrite was retarded by addition of phosphate and silicate. The retardation of pyrite oxidation was probably due to coating of insoluble materials on the pyrite surface.
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spelling upm.eprints-105492024-04-17T01:08:44Z http://psasir.upm.edu.my/id/eprint/10549/ Characterization and Amelioration of Selected Acid Sulfate Soils in Malaysia Sarwani, Muhrizal Researchers in the past had focused their study on the common or standard acid sulfate soils, which are characterized by high iron and the presence of jarosite mottles. Little is known about the characteristics and management of iron-poor acid sulfate soils and this study was conducted to provide the dearth of information. This study aimed to characterize and ameliorate acid sulfate soils in Malaysia. Three common acid sulfate soils in Malaysia namely Teluk, Jawa and Linau series were investigated in three phases. The first phase was concentrated on the characterization of the soils. The second phase dealt with laboratory incubation experiments to study oxidation processes. The third phase was on the ameliorative effects of organic materials, lime, phosphate and silicate application on acid sulfate soils. Results of the study revealed the presence of both iron-rich and iron-poor acid sulfate soils in Malaysia. The former, represented by the Teluk and Jawa soils, had thick accumulation of iron in the B-horizon. They followed the standard morphological profile commonly found under tropical monsoon climate. The latter, represented by the Linau soil, was low in iron content in the B-horizon. They followed the standard morphological profile commonly found under tropical monsoon climate. The latter, represented by the Linau soil, was low in iron content in the B-horizon. The low content of iron was most probably due to high organic content enhanced by wet climate in Malaysia. The formation of Fe (III) oxide was hindered when the environment was rich in organics. Incubation study indicated that oxidation of pyrite resulted in a decrease in pH and the formation of jarosite which, in tum, transformed into short-range order Fe-oxides. The yellow mottles formed during pyrite oxidation were jarosite/natrojarosite and alunite as detected by X-ray diffraction analysis. The oxidation of pyrite was retarded by addition of phosphate and silicate. The retardation of pyrite oxidation was probably due to coating of insoluble materials on the pyrite surface. 2001-07 Thesis NonPeerReviewed text en http://psasir.upm.edu.my/id/eprint/10549/1/FP_2001_9.pdf Sarwani, Muhrizal (2001) Characterization and Amelioration of Selected Acid Sulfate Soils in Malaysia. Doctoral thesis, Universiti Putra Malaysia. Acid sulphate soils - Malaysia - Case studies English
spellingShingle Acid sulphate soils - Malaysia - Case studies
Sarwani, Muhrizal
Characterization and Amelioration of Selected Acid Sulfate Soils in Malaysia
title Characterization and Amelioration of Selected Acid Sulfate Soils in Malaysia
title_full Characterization and Amelioration of Selected Acid Sulfate Soils in Malaysia
title_fullStr Characterization and Amelioration of Selected Acid Sulfate Soils in Malaysia
title_full_unstemmed Characterization and Amelioration of Selected Acid Sulfate Soils in Malaysia
title_short Characterization and Amelioration of Selected Acid Sulfate Soils in Malaysia
title_sort characterization and amelioration of selected acid sulfate soils in malaysia
topic Acid sulphate soils - Malaysia - Case studies
url http://psasir.upm.edu.my/id/eprint/10549/1/FP_2001_9.pdf
work_keys_str_mv AT sarwanimuhrizal characterizationandameliorationofselectedacidsulfatesoilsinmalaysia