Increase in Raw Milk Demand and Its Long-Run Effects on Dairy Industrial Organization in Taiwan-An Approach with Spatial Equilibrium Analysis- - 九大コレクション

＜紀要論文＞
Increase in Raw Milk Demand and Its Long-Run Effects on Dairy Industrial Organization in Taiwan-An Approach with Spatial Equilibrium Analysis-

作成者	作成者名 Lin, Lily 所属機関所属機関名 Department of Agricultural Economies, Facluty of Agriculture, Kyushu University
作成者	著者識別子 K000332 作成者名 Kawaguchi, Tsunemasa 川口, 雅正所属機関所属機関名 Department of Agricultural Economies, Facluty of Agriculture, Kyushu University 九州大学農学部農政経済学科農業計算学講座
本文言語	英語
出版者	Kyushu University
出版者	九州大学農学部
発行日	1999-02
収録物名	九州大学大学院農学研究院紀要
巻	43
号	3/4
開始ページ	509
終了ページ	529
出版タイプ	Version of Record
アクセス権	open access
Crossref DOI	https://doi.org/10.5109/24298
関連DOI	九州大学農学部紀要 \|\| 43(3/4) \|\| p509-529
	Journal of the Faculty of Agriculture, Kyushu University \|\| 43(3/4) \|\| p509-529
	http://www.agr.kyushu-u.ac.jp/
関連URI	九州大学農学部紀要 \|\| 43(3/4) \|\| p509-529
	Journal of the Faculty of Agriculture, Kyushu University \|\| 43(3/4) \|\| p509-529
	http://www.agr.kyushu-u.ac.jp/
関連情報	九州大学農学部紀要 \|\| 43(3/4) \|\| p509-529
	Journal of the Faculty of Agriculture, Kyushu University \|\| 43(3/4) \|\| p509-529
	http://www.agr.kyushu-u.ac.jp/

ファイル	ファイルタイプ	サイズ	閲覧回数	説明
p509	pdf	5.45 MB	496

PISSN	0023-6152
NCID	AA00697606
レコードID	24298
査読有無	査読無
主題	Fluid milk
	Taiwanese dairy industry
	Spatial equilibrium analysis
ISSN	0023-6152
NCID	AA00697606
注記	We devised an experimental apparatus to simulate the electroosmotic and hydraulic flow of water during electrokinetic soil decontamination process. The apparatus is an open box with electrode compartments at the both ends and a central compartment in which soil sample is packed. A laminated wire gauze-nylon net was used as cathod-cum-scparator. The opening of the wire gauze should be> 1 mm to let evolved gas escape freely. The carthode compartment was filled with water and a graphite rod immersed wherein was used as the a node. The draining conduit was attached to the cathodic end at a position lower than the water table in the anode compartment. Under this setup, the electroosmotie and hydraulic flow contributes to the water flow through the soil. To evaluate the electroosmmie flow, the flow under zero electric field was subtracted from the total water flow. Experiments with a soil with mixed mineralogy showed the subtraction method gave fairly reproducible results with respect to the rate of electroosmotie flow.
登録日	2012.08.02
更新日	2022.11.11