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ABOUT RENDZINA SOILS WHICH IS FORMED ON GYPSUM FROM SLON DEPRESSION


 
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1. Title Title of document ABOUT RENDZINA SOILS WHICH IS FORMED ON GYPSUM FROM SLON DEPRESSION
 
2. Creator Author's name, affiliation, country M. Parichi
 
2. Creator Author's name, affiliation, country Anca-Luiza Stănilă
 
2. Creator Author's name, affiliation, country V. Duca
 
2. Creator Author's name, affiliation, country Nineta Rizea
 
3. Subject Discipline(s)
 
3. Subject Keyword(s)
 
4. Description Abstract By now, in our country wasn ׳ t separated areas with exclusit rendzine gypsom.
In most cases, these types of soils apear in association with other soils. We found rendzina
and cambic rendzina in upper basin of Drajna valley witch, is locate on mountain-hill
morphological contact and limited from cast by Pintenul de Homorâciu (Paleogen
structure). These soils are possibly, to represent on maps. On large areas appear only
cambic rendzina in various conditions of slopes. Analytic data about these soil indicate a
large content of cley (52-56 per cent), neutral reaction middle-large cation exchange
capacity (34-49 me/100 g soil) and middle-large humus content.
 
5. Publisher Organizing agency, location Editura Universit??ii "Alexandru Ion Cuza"
 
6. Contributor Sponsor(s)
 
7. Date (YYYY-MM-DD) 2012-03-08
 
8. Type Status & genre Peer-reviewed Article
 
8. Type Type
 
9. Format File format PDF
 
10. Identifier Uniform Resource Identifier http://factori.soilscience.ro/index.php/fspdzt/article/view/319
 
10. Identifier Digital Object Identifier (DOI) http://dx.doi.org/10.15551/fppzt.v4i1.319
 
11. Source Title; vol., no. (year) Soil Forming Factors and Processes from the Temperate Zone; Vol 4, No 1 (2005)
 
12. Language English=en
 
13. Relation Supp. Files
 
14. Coverage Geo-spatial location, chronological period, research sample (gender, age, etc.)
 
15. Rights Copyright and permissions Copyright (c)