Articolul precedent |
Articolul urmator |
228 0 |
SM ISO690:2012 КOЛЬВEНКO, В., МУНТЯН, А.. Динaмикa тeмпepaтypы пoчвы в гopизoнтe 0,2-3,2м зa пepиoд 1993-2013гг. Пo дaнным мeтeocтaнции "Тиpacпoль". In: Mediul şi dezvoltarea durabilă,: conferinţă ştiinţifică naţională cu participare internaţională, 6-8 octombrie 2016, Chişinău. Chişinău: Tipografia UST, 2016, Ediţia 3, pp. 187-190. ISBN 978-9975-76-170-3. |
EXPORT metadate: Google Scholar Crossref CERIF DataCite Dublin Core |
Mediul şi dezvoltarea durabilă, Ediţia 3, 2016 |
||||||
Conferința "Mediul şi dezvoltarea durabilă, " Chişinău, Moldova, 6-8 octombrie 2016 | ||||||
|
||||||
Pag. 187-190 | ||||||
|
||||||
Descarcă PDF | ||||||
Rezumat | ||||||
The work describes the dynamics of soil temperature at a depth of 0,20, 0,40, 0,80, 1,2, 1,6, 2,4, 3,2 meter for the period 1993-2013 with the aim of assessing changes in soil temperature the number of continuous observations at the weather station Tiraspol. Was built linear trends for each studied horizon. A comparison of years of soil temperature on bare and natural cover of the soil at a depth of 0.2 m |
||||||
|
Cerif XML Export
<?xml version='1.0' encoding='utf-8'?> <CERIF xmlns='urn:xmlns:org:eurocris:cerif-1.5-1' xsi:schemaLocation='urn:xmlns:org:eurocris:cerif-1.5-1 http://www.eurocris.org/Uploads/Web%20pages/CERIF-1.5/CERIF_1.5_1.xsd' xmlns:xsi='http://www.w3.org/2001/XMLSchema-instance' release='1.5' date='2012-10-07' sourceDatabase='Output Profile'> <cfResPubl> <cfResPublId>ibn-ResPubl-159836</cfResPublId> <cfResPublDate>2016</cfResPublDate> <cfVol>Ediţia 3</cfVol> <cfStartPage>187</cfStartPage> <cfISBN>978-9975-76-170-3</cfISBN> <cfURI>https://ibn.idsi.md/ro/vizualizare_articol/159836</cfURI> <cfTitle cfLangCode='RU' cfTrans='o'>Динaмикa тeмпepaтypы пoчвы в гopизoнтe 0,2-3,2м зa пepиoд 1993-2013гг. Пo дaнным мeтeocтaнции "Тиpacпoль"</cfTitle> <cfAbstr cfLangCode='EN' cfTrans='o'><p><em>The work describes the dynamics of soil temperature at a depth of 0,20, 0,40, 0,80, 1,2, 1,6, 2,4, 3,2 meter for the period 1993-2013 with the aim of assessing changes in soil temperature the number of continuous observations at the weather station Tiraspol. Was built linear trends for each studied horizon. A comparison of years of soil temperature on bare and natural cover of the soil at a depth of 0.2 m</em></p></cfAbstr> <cfResPubl_Class> <cfClassId>eda2d9e9-34c5-11e1-b86c-0800200c9a66</cfClassId> <cfClassSchemeId>759af938-34ae-11e1-b86c-0800200c9a66</cfClassSchemeId> <cfStartDate>2016T24:00:00</cfStartDate> </cfResPubl_Class> <cfResPubl_Class> <cfClassId>e601872f-4b7e-4d88-929f-7df027b226c9</cfClassId> <cfClassSchemeId>40e90e2f-446d-460a-98e5-5dce57550c48</cfClassSchemeId> <cfStartDate>2016T24:00:00</cfStartDate> </cfResPubl_Class> <cfPers_ResPubl> <cfPersId>ibn-person-90936</cfPersId> <cfClassId>49815870-1cfe-11e1-8bc2-0800200c9a66</cfClassId> <cfClassSchemeId>b7135ad0-1d00-11e1-8bc2-0800200c9a66</cfClassSchemeId> <cfStartDate>2016T24:00:00</cfStartDate> </cfPers_ResPubl> <cfPers_ResPubl> <cfPersId>ibn-person-80430</cfPersId> <cfClassId>49815870-1cfe-11e1-8bc2-0800200c9a66</cfClassId> <cfClassSchemeId>b7135ad0-1d00-11e1-8bc2-0800200c9a66</cfClassSchemeId> <cfStartDate>2016T24:00:00</cfStartDate> </cfPers_ResPubl> </cfResPubl> <cfPers> <cfPersId>ibn-Pers-90936</cfPersId> <cfPersName_Pers> <cfPersNameId>ibn-PersName-90936-1</cfPersNameId> <cfClassId>55f90543-d631-42eb-8d47-d8d9266cbb26</cfClassId> <cfClassSchemeId>7375609d-cfa6-45ce-a803-75de69abe21f</cfClassSchemeId> <cfStartDate>2016T24:00:00</cfStartDate> <cfFamilyNames>Кoльвeнкo</cfFamilyNames> <cfFirstNames>В.</cfFirstNames> </cfPersName_Pers> </cfPers> <cfPers> <cfPersId>ibn-Pers-80430</cfPersId> <cfPersName_Pers> <cfPersNameId>ibn-PersName-80430-1</cfPersNameId> <cfClassId>55f90543-d631-42eb-8d47-d8d9266cbb26</cfClassId> <cfClassSchemeId>7375609d-cfa6-45ce-a803-75de69abe21f</cfClassSchemeId> <cfStartDate>2016T24:00:00</cfStartDate> <cfFamilyNames>Мунтян</cfFamilyNames> <cfFirstNames>А.</cfFirstNames> </cfPersName_Pers> </cfPers> </CERIF>