Effect of different temperature on burning peat soil / Amir Nur Rahim Abd Aziz

Smoldering wildfires propagate slowly through surface of organic layers of the soil and severely affect the soil, producing physical, chemical and biological changes. These effects are caused by the prolonged heating and the large loss of soil mass and chemical properties are documented in the liter...

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Main Author:	Abd Aziz, Amir Nur Rahim
Format:	Student Project
Language:	English
Published:	Faculty of Plantation and Agrotechnology 2015
Online Access:	http://ir.uitm.edu.my/id/eprint/16906/ http://ir.uitm.edu.my/id/eprint/16906/2/PPb_AMIR%20NUR%20RAHIM%20ABD%20AZIZ%20AT%2015_5.pdf

id	uitm-16906
recordtype	eprints
spelling	uitm-169062019-05-04T14:18:34Z http://ir.uitm.edu.my/id/eprint/16906/ Effect of different temperature on burning peat soil / Amir Nur Rahim Abd Aziz Abd Aziz, Amir Nur Rahim Smoldering wildfires propagate slowly through surface of organic layers of the soil and severely affect the soil, producing physical, chemical and biological changes. These effects are caused by the prolonged heating and the large loss of soil mass and chemical properties are documented in the literature. This paper attempts to understand the effect of different temperature on peat soil (without burning, 100°c, 200°c, 300°c, 400°c, and 500°c) on volume soil loss, nutrient (N, P, K, Mg, Ca, Mn) and pH. 18 samples treatments are test and 3 replication for each temperature. The soil sample obtains at Felcra seri Mendapat and the analysis is done at UiTM Jasin Laboratory. Volume of soil loss is record after bum in Muffle Furnace. In addition, the nutrient analysis tests with ICP-OES (Inductively Couple Plasma-Optical Emission Spectrometry) for each of temperature. In order to analyse the nutrient, the sample were extracted first. For the third test, is performing using pH meter with the appropriate electrode. Volume soil loss, nutrient, and pH showed different response towards different temperature. Peat volumes will be lost since the fire consumed the peat soil. This result decreases the depth of plant soil due to conversion of organic matter to carbon dioxide (C0²). The pH of peat soil also shows the trend of increasing, but in moderate increasing. Finally, the regenerative aspect of different temperature is discussed. Faculty of Plantation and Agrotechnology 2015 Student Project NonPeerReviewed text en http://ir.uitm.edu.my/id/eprint/16906/2/PPb_AMIR%20NUR%20RAHIM%20ABD%20AZIZ%20AT%2015_5.pdf Abd Aziz, Amir Nur Rahim (2015) Effect of different temperature on burning peat soil / Amir Nur Rahim Abd Aziz. [Student Project] (Unpublished)
repository_type	Digital Repository
institution_category	Local University
institution	Universiti Teknologi MARA
building	UiTM Institutional Repository
collection	Online Access
language	English
description	Smoldering wildfires propagate slowly through surface of organic layers of the soil and severely affect the soil, producing physical, chemical and biological changes. These effects are caused by the prolonged heating and the large loss of soil mass and chemical properties are documented in the literature. This paper attempts to understand the effect of different temperature on peat soil (without burning, 100°c, 200°c, 300°c, 400°c, and 500°c) on volume soil loss, nutrient (N, P, K, Mg, Ca, Mn) and pH. 18 samples treatments are test and 3 replication for each temperature. The soil sample obtains at Felcra seri Mendapat and the analysis is done at UiTM Jasin Laboratory. Volume of soil loss is record after bum in Muffle Furnace. In addition, the nutrient analysis tests with ICP-OES (Inductively Couple Plasma-Optical Emission Spectrometry) for each of temperature. In order to analyse the nutrient, the sample were extracted first. For the third test, is performing using pH meter with the appropriate electrode. Volume soil loss, nutrient, and pH showed different response towards different temperature. Peat volumes will be lost since the fire consumed the peat soil. This result decreases the depth of plant soil due to conversion of organic matter to carbon dioxide (C0²). The pH of peat soil also shows the trend of increasing, but in moderate increasing. Finally, the regenerative aspect of different temperature is discussed.
format	Student Project
author	Abd Aziz, Amir Nur Rahim
spellingShingle	Abd Aziz, Amir Nur Rahim Effect of different temperature on burning peat soil / Amir Nur Rahim Abd Aziz
author_facet	Abd Aziz, Amir Nur Rahim
author_sort	Abd Aziz, Amir Nur Rahim
title	Effect of different temperature on burning peat soil / Amir Nur Rahim Abd Aziz
title_short	Effect of different temperature on burning peat soil / Amir Nur Rahim Abd Aziz
title_full	Effect of different temperature on burning peat soil / Amir Nur Rahim Abd Aziz
title_fullStr	Effect of different temperature on burning peat soil / Amir Nur Rahim Abd Aziz
title_full_unstemmed	Effect of different temperature on burning peat soil / Amir Nur Rahim Abd Aziz
title_sort	effect of different temperature on burning peat soil / amir nur rahim abd aziz
publisher	Faculty of Plantation and Agrotechnology
publishDate	2015
url	http://ir.uitm.edu.my/id/eprint/16906/ http://ir.uitm.edu.my/id/eprint/16906/2/PPb_AMIR%20NUR%20RAHIM%20ABD%20AZIZ%20AT%2015_5.pdf
first_indexed	2023-09-18T22:57:08Z
last_indexed	2023-09-18T22:57:08Z
_version_	1777417928644231168

Effect of different temperature on burning peat soil / Amir Nur Rahim Abd Aziz

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