Reaksi Pemasaman Senyawa Pirit pada Tanah Rawa Pasang Surut

Acidity Reaction of Pyrite in Tidal Swampland (B.J. Priatmadi and A. Haris): Most of swamp soils in tidal landare Acid Sulfate Soils. Acid sulfate soils are the common name given to soils containing iron sulfides (pyrite). Thesoils are characterized by very low pH and high amount of soluble S and Fe...
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Autor*in:	Bambang Joko Priatmadi [verfasserIn] Abdul Haris [verfasserIn]

Format:	E-Artikel
Sprache:	Englisch ; Indonesisch

Erschienen:	2009

Schlagwörter:	Acid sulfate soils pyrite soil acidity

Übergeordnetes Werk:	In: Journal of Tropical Soils - University of Lampung, 2017, 14(2009), 1, Seite 19-24
Übergeordnetes Werk:	volume:14 ; year:2009 ; number:1 ; pages:19-24

Links:	Link aufrufen Link aufrufen Journal toc Journal toc

Katalog-ID:	DOAJ045421625

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520			\|a Acidity Reaction of Pyrite in Tidal Swampland (B.J. Priatmadi and A. Haris): Most of swamp soils in tidal landare Acid Sulfate Soils. Acid sulfate soils are the common name given to soils containing iron sulfides (pyrite). Thesoils are characterized by very low pH and high amount of soluble S and Fe, resulted from oxidation of pyrite whensoils are drained. This study was aimed to determine acidity pattern, iron and sulfate solubility as the impact of thelength time of oxidized, the effect of inhibitors application to acidity rate of sulfidic materials and top soils. Thematerials are: (1) soils at pyritic layer (sulfidic materials) and (2) soils at 0 – 20 cm from soil surface. Soils issampled at Barambai reclaimed area, Barito Kuala Regency, South Kalimantan Province. In the laboratory soilstreated with some ameliorants, that are silica, phosphate and lime applied with dosage 2 t ha-1 with 3 replicationstimes. The soils incubated for 2 weeks under submerged condition. After soil incubation, soil exposed to the air for1 week, 2 weeks, 4 weeks, and 6 weeks. Parameters of soil analysis include pH, sulfate and iron soluble. Results ofthis study showed that (1) soil acidity rate of sulfidic materials more faster than upper soils when soils and sulfidicmaterials oxidized intensively, (2) at submerged soil condition or high soil water content, the application of ameliorantseffective increasing the soil pH of the upper soils, (3) at further oxidized soil condition or lower soil water content,the application of ameliorants inhibited acidity rate of soils and sulfidic materials, and (4) at further oxidized soilcondition or lower soil water content, the application of ameliorants increased iron solubility of soils and sulfidicmaterials.
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callnumber-first	Q - Science
author	Bambang Joko Priatmadi
spellingShingle	Bambang Joko Priatmadi misc Q1-390 misc Acid sulfate soils misc pyrite misc soil acidity misc Science (General) Reaksi Pemasaman Senyawa Pirit pada Tanah Rawa Pasang Surut
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topic_title	Q1-390 Reaksi Pemasaman Senyawa Pirit pada Tanah Rawa Pasang Surut Acid sulfate soils pyrite soil acidity
topic	misc Q1-390 misc Acid sulfate soils misc pyrite misc soil acidity misc Science (General)
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title	Reaksi Pemasaman Senyawa Pirit pada Tanah Rawa Pasang Surut
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title_sort	reaksi pemasaman senyawa pirit pada tanah rawa pasang surut
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title_auth	Reaksi Pemasaman Senyawa Pirit pada Tanah Rawa Pasang Surut
abstract	Acidity Reaction of Pyrite in Tidal Swampland (B.J. Priatmadi and A. Haris): Most of swamp soils in tidal landare Acid Sulfate Soils. Acid sulfate soils are the common name given to soils containing iron sulfides (pyrite). Thesoils are characterized by very low pH and high amount of soluble S and Fe, resulted from oxidation of pyrite whensoils are drained. This study was aimed to determine acidity pattern, iron and sulfate solubility as the impact of thelength time of oxidized, the effect of inhibitors application to acidity rate of sulfidic materials and top soils. Thematerials are: (1) soils at pyritic layer (sulfidic materials) and (2) soils at 0 – 20 cm from soil surface. Soils issampled at Barambai reclaimed area, Barito Kuala Regency, South Kalimantan Province. In the laboratory soilstreated with some ameliorants, that are silica, phosphate and lime applied with dosage 2 t ha-1 with 3 replicationstimes. The soils incubated for 2 weeks under submerged condition. After soil incubation, soil exposed to the air for1 week, 2 weeks, 4 weeks, and 6 weeks. Parameters of soil analysis include pH, sulfate and iron soluble. Results ofthis study showed that (1) soil acidity rate of sulfidic materials more faster than upper soils when soils and sulfidicmaterials oxidized intensively, (2) at submerged soil condition or high soil water content, the application of ameliorantseffective increasing the soil pH of the upper soils, (3) at further oxidized soil condition or lower soil water content,the application of ameliorants inhibited acidity rate of soils and sulfidic materials, and (4) at further oxidized soilcondition or lower soil water content, the application of ameliorants increased iron solubility of soils and sulfidicmaterials.
abstractGer	Acidity Reaction of Pyrite in Tidal Swampland (B.J. Priatmadi and A. Haris): Most of swamp soils in tidal landare Acid Sulfate Soils. Acid sulfate soils are the common name given to soils containing iron sulfides (pyrite). Thesoils are characterized by very low pH and high amount of soluble S and Fe, resulted from oxidation of pyrite whensoils are drained. This study was aimed to determine acidity pattern, iron and sulfate solubility as the impact of thelength time of oxidized, the effect of inhibitors application to acidity rate of sulfidic materials and top soils. Thematerials are: (1) soils at pyritic layer (sulfidic materials) and (2) soils at 0 – 20 cm from soil surface. Soils issampled at Barambai reclaimed area, Barito Kuala Regency, South Kalimantan Province. In the laboratory soilstreated with some ameliorants, that are silica, phosphate and lime applied with dosage 2 t ha-1 with 3 replicationstimes. The soils incubated for 2 weeks under submerged condition. After soil incubation, soil exposed to the air for1 week, 2 weeks, 4 weeks, and 6 weeks. Parameters of soil analysis include pH, sulfate and iron soluble. Results ofthis study showed that (1) soil acidity rate of sulfidic materials more faster than upper soils when soils and sulfidicmaterials oxidized intensively, (2) at submerged soil condition or high soil water content, the application of ameliorantseffective increasing the soil pH of the upper soils, (3) at further oxidized soil condition or lower soil water content,the application of ameliorants inhibited acidity rate of soils and sulfidic materials, and (4) at further oxidized soilcondition or lower soil water content, the application of ameliorants increased iron solubility of soils and sulfidicmaterials.
abstract_unstemmed	Acidity Reaction of Pyrite in Tidal Swampland (B.J. Priatmadi and A. Haris): Most of swamp soils in tidal landare Acid Sulfate Soils. Acid sulfate soils are the common name given to soils containing iron sulfides (pyrite). Thesoils are characterized by very low pH and high amount of soluble S and Fe, resulted from oxidation of pyrite whensoils are drained. This study was aimed to determine acidity pattern, iron and sulfate solubility as the impact of thelength time of oxidized, the effect of inhibitors application to acidity rate of sulfidic materials and top soils. Thematerials are: (1) soils at pyritic layer (sulfidic materials) and (2) soils at 0 – 20 cm from soil surface. Soils issampled at Barambai reclaimed area, Barito Kuala Regency, South Kalimantan Province. In the laboratory soilstreated with some ameliorants, that are silica, phosphate and lime applied with dosage 2 t ha-1 with 3 replicationstimes. The soils incubated for 2 weeks under submerged condition. After soil incubation, soil exposed to the air for1 week, 2 weeks, 4 weeks, and 6 weeks. Parameters of soil analysis include pH, sulfate and iron soluble. Results ofthis study showed that (1) soil acidity rate of sulfidic materials more faster than upper soils when soils and sulfidicmaterials oxidized intensively, (2) at submerged soil condition or high soil water content, the application of ameliorantseffective increasing the soil pH of the upper soils, (3) at further oxidized soil condition or lower soil water content,the application of ameliorants inhibited acidity rate of soils and sulfidic materials, and (4) at further oxidized soilcondition or lower soil water content, the application of ameliorants increased iron solubility of soils and sulfidicmaterials.
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title_short	Reaksi Pemasaman Senyawa Pirit pada Tanah Rawa Pasang Surut
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up_date	2024-07-03T14:53:18.110Z
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