Tenth International Course on Land Drainage-Chapter 2.5 1971

dc.contributor.corpauthor	Kenya Agricultural Research Institute
dc.date.accessioned	2015-08-10T09:32:44Z
dc.date.available	2015-08-10T09:32:44Z
dc.date.issued	1971	en
dc.description.abstract	As peat is accumulated organic material it is only formed at places where the quantity of organic matter grown in a certain period exceeds the quantity of organic matter decayed in the same period. Water always plays an important role in peat formation: because it works as a preservative against decay. In wet climates areas with a poor natural drainage – lowest parts, gentle or no slope - may have peat growth, In the temperate zone peat is rather common 1 e.g. in Ireland, Great Britain, Holland, Germany, Poland and the northern isles of Japan,	en
dc.format.pages	25	en
dc.identifier.uri	http://localhost:8080/dspace/handle/0/8829
dc.language.iso	en	en
dc.publisher	Kenya Agriculture Research Institute	en
dc.publisher.place	Nairobi	en
dc.rights.uri	http://creativecommons.org/licenses/by/3.0/	en
dc.subject.agrovoc	Drainage	en
dc.subject.agrovoc	Acid sulphate soils	en
dc.subject.agrovoc	Acidification	en
dc.subject.agrovoc	Fields	en
dc.subject.agrovoc	Climate	en
dc.subject.agrovoc	Soil mechanics	en
dc.title	Tenth International Course on Land Drainage-Chapter 2.5 1971	en
dc.type	Book	*
dc.type.refereed	Refereed	en
dc.type.specified	Article	en

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