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Interaction fugacity model for water, sediment and seagrass

Fugacity concept is convenient in environmental chemical equilibrium. Mathematical model for simulation of chemical movement in the estuary consists of 3 compartments which are water, sediment, and seagrass. The influence factors at site location such as area, depth, volume, mass of water, mass of s...

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Main Authors:	Ahmad, F., Azman, S., Said, M. I. M., Hamid, N. H. A., Harun, H., Awang, M., Rahman, M. A. A.
Format:	Article
Published:	Blue Eyes Intelligence Engineering and Sciences Publication 2019
Subjects:	TA Engineering (General). Civil engineering (General)
Online Access:	http://eprints.utm.my/id/eprint/90741/ https://www.ijitee.org/wp-content/uploads/papers/v8i8s/H10700688S19.pdf.
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id	my.utm.90741
record_format	eprints
spelling	my.utm.907412021-04-29T23:48:57Z http://eprints.utm.my/id/eprint/90741/ Interaction fugacity model for water, sediment and seagrass Ahmad, F. Azman, S. Said, M. I. M. Hamid, N. H. A. Harun, H. Awang, M. Rahman, M. A. A. TA Engineering (General). Civil engineering (General) Fugacity concept is convenient in environmental chemical equilibrium. Mathematical model for simulation of chemical movement in the estuary consists of 3 compartments which are water, sediment, and seagrass. The influence factors at site location such as area, depth, volume, mass of water, mass of sediment, mass of seagrass, and current water flow were identified. The current water flow at Pulai River Estuary was measured in order to identify the allowable distance from mouth of Pulai River to Pulaiseagrass bed. The average wind speed can be found from World Weather and Climate information, 2015. The estimation method is practically used for getting the approximate estimation of concentration in each medium. The ratio of the concentration in each medium is called ‘concentration factor’. The ratio between seawater and sediment is 1: 1.439 x 10-3; ratio between sediment and seagrass is1: 4.25 x 10-9; and the ratio between seawater and seagrass is 1: 6.11x 10-12 C3. Thus, quantitative water, sediment and seagrass fugacity/ aquivalence mass balance model was developed for Pulai River Estuary is relevant. Blue Eyes Intelligence Engineering and Sciences Publication 2019-06 Article PeerReviewed Ahmad, F. and Azman, S. and Said, M. I. M. and Hamid, N. H. A. and Harun, H. and Awang, M. and Rahman, M. A. A. (2019) Interaction fugacity model for water, sediment and seagrass. International Journal of Innovative Technology and Exploring Engineering, 8 (9). pp. 406-410. ISSN 2278-3075 https://www.ijitee.org/wp-content/uploads/papers/v8i8s/H10700688S19.pdf.
institution	Universiti Teknologi Malaysia
building	UTM Library
collection	Institutional Repository
continent	Asia
country	Malaysia
content_provider	Universiti Teknologi Malaysia
content_source	UTM Institutional Repository
url_provider	http://eprints.utm.my/
topic	TA Engineering (General). Civil engineering (General)
spellingShingle	TA Engineering (General). Civil engineering (General) Ahmad, F. Azman, S. Said, M. I. M. Hamid, N. H. A. Harun, H. Awang, M. Rahman, M. A. A. Interaction fugacity model for water, sediment and seagrass
description	Fugacity concept is convenient in environmental chemical equilibrium. Mathematical model for simulation of chemical movement in the estuary consists of 3 compartments which are water, sediment, and seagrass. The influence factors at site location such as area, depth, volume, mass of water, mass of sediment, mass of seagrass, and current water flow were identified. The current water flow at Pulai River Estuary was measured in order to identify the allowable distance from mouth of Pulai River to Pulaiseagrass bed. The average wind speed can be found from World Weather and Climate information, 2015. The estimation method is practically used for getting the approximate estimation of concentration in each medium. The ratio of the concentration in each medium is called ‘concentration factor’. The ratio between seawater and sediment is 1: 1.439 x 10-3; ratio between sediment and seagrass is1: 4.25 x 10-9; and the ratio between seawater and seagrass is 1: 6.11x 10-12 C3. Thus, quantitative water, sediment and seagrass fugacity/ aquivalence mass balance model was developed for Pulai River Estuary is relevant.
format	Article
author	Ahmad, F. Azman, S. Said, M. I. M. Hamid, N. H. A. Harun, H. Awang, M. Rahman, M. A. A.
author_facet	Ahmad, F. Azman, S. Said, M. I. M. Hamid, N. H. A. Harun, H. Awang, M. Rahman, M. A. A.
author_sort	Ahmad, F.
title	Interaction fugacity model for water, sediment and seagrass
title_short	Interaction fugacity model for water, sediment and seagrass
title_full	Interaction fugacity model for water, sediment and seagrass
title_fullStr	Interaction fugacity model for water, sediment and seagrass
title_full_unstemmed	Interaction fugacity model for water, sediment and seagrass
title_sort	interaction fugacity model for water, sediment and seagrass
publisher	Blue Eyes Intelligence Engineering and Sciences Publication
publishDate	2019
url	http://eprints.utm.my/id/eprint/90741/ https://www.ijitee.org/wp-content/uploads/papers/v8i8s/H10700688S19.pdf.
_version_	1698696978839371776
score	13.211869

Interaction fugacity model for water, sediment and seagrass

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