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		<identifier>oai:zbc.uz.zgora.pl:45369</identifier>
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<dc:title xml:lang="en"><![CDATA[The unfrozen water content in faozen cohesive soils in the light of DSC results = Zawartość wody niezamarzniętej w zamarzniętych gruntach spoistych w świetle wyników otrzymanych przy użyciu kalorymetrii skaningowej DSC]]></dc:title>
<dc:title xml:lang="pl"><![CDATA[The unfrozen water content in faozen cohesive soils in the light of DSC results = Zawartość wody niezamarzniętej w zamarzniętych gruntach spoistych w świetle wyników otrzymanych przy użyciu kalorymetrii skaningowej DSC]]></dc:title>
<dc:creator><![CDATA[Kozłowski, Tomasz]]></dc:creator>
<dc:subject xml:lang="en"><![CDATA[X jubileuszowe sympozjum glacitektoniki]]></dc:subject>
<dc:subject xml:lang="pl"><![CDATA[X jubileuszowe sympozjum glacitektoniki]]></dc:subject>
<dc:description xml:lang="en"><![CDATA[Results of determination of the unfrozen water function in frozen soil-water system involving analysis of the DSC signal in terms of convolution has been presented. Analysis of the obtained results suggests that the process of the ice melting in the soil-water system is not a continuous phase change.]]></dc:description>
<dc:description xml:lang="en"><![CDATA[The existence of five separate stages of the phase change process during warming from -28°C has been indicated. Three of them, I, II and V, are characterised by quite a vanishing of the phase effects. The intensity of the phase effects during stage IV near the melting point Tr is almost two orders of magnitude grearer than in the low-temperature stage II.]]></dc:description>
<dc:description xml:lang="en"><![CDATA[Additionally, many micro-stages without any phase changes were observed and among them, a characteristic significant stage III directly before the final melting called "the plateau".]]></dc:description>
<dc:description xml:lang="en"><![CDATA[nr 5-11 tytuł: Politechnika Zielonogórska - Zeszyty Naukowe]]></dc:description>
<dc:description xml:lang="en"><![CDATA[nr 1-4 tytuł: Wyższa Szkoła Inżynierska im. Jurija Gagarina w Zielonej Górze - Zeszyty Naukowe]]></dc:description>
<dc:description xml:lang="en"><![CDATA[seria główna: Zeszyty Naukowe]]></dc:description>
<dc:description xml:lang="en"><![CDATA[zeszyt 14 ukazał się jako nr 134 serii głównej]]></dc:description>
<dc:description xml:lang="pl"><![CDATA[Results of determination of the unfrozen water function in frozen soil-water system involving analysis of the DSC signal in terms of convolution has been presented. Analysis of the obtained results suggests that the process of the ice melting in the soil-water system is not a continuous phase change.]]></dc:description>
<dc:description xml:lang="pl"><![CDATA[The existence of five separate stages of the phase change process during warming from -28°C has been indicated. Three of them, I, II and V, are characterised by quite a vanishing of the phase effects. The intensity of the phase effects during stage IV near the melting point Tr is almost two orders of magnitude grearer than in the low-temperature stage II.]]></dc:description>
<dc:description xml:lang="pl"><![CDATA[Additionally, many micro-stages without any phase changes were observed and among them, a characteristic significant stage III directly before the final melting called "the plateau".]]></dc:description>
<dc:description xml:lang="pl"><![CDATA[nr 5-11 tytuł: Politechnika Zielonogórska - Zeszyty Naukowe]]></dc:description>
<dc:description xml:lang="pl"><![CDATA[nr 1-4 tytuł: Wyższa Szkoła Inżynierska im. Jurija Gagarina w Zielonej Górze - Zeszyty Naukowe]]></dc:description>
<dc:description xml:lang="pl"><![CDATA[seria główna: Zeszyty Naukowe]]></dc:description>
<dc:description xml:lang="pl"><![CDATA[zeszyt 14 ukazał się jako nr 134 serii głównej]]></dc:description>
<dc:publisher><![CDATA[Zielona Góra: Oficyna Wydawnicza Uniwersytetu Zielonogórskiego]]></dc:publisher>
<dc:contributor><![CDATA[Gontaszewska-Piekarz, Agnieszka - red.]]></dc:contributor>
<dc:date><![CDATA[2007]]></dc:date>
<dc:type xml:lang="en"><![CDATA[artykuł]]></dc:type>
<dc:type xml:lang="pl"><![CDATA[artykuł]]></dc:type>
<dc:format xml:lang="en"><![CDATA[application/pdf]]></dc:format>
<dc:format xml:lang="pl"><![CDATA[application/pdf]]></dc:format>
<dc:identifier><![CDATA[http://www.zbc.uz.zgora.pl/repozytorium/Content/45369/PDF/9_kozlowski_zawartosc.pdf]]></dc:identifier>
<dc:identifier><![CDATA[https://zbc.uz.zgora.pl/repozytorium/dlibra/publication/51600/edition/45369/content]]></dc:identifier>
<dc:identifier><![CDATA[oai:zbc.uz.zgora.pl:45369]]></dc:identifier>
<dc:source xml:lang="en"><![CDATA[Zeszyty Naukowe Uniwersytetu Zielonogórskiego, Tom 14]]></dc:source>
<dc:source xml:lang="pl"><![CDATA[Zeszyty Naukowe Uniwersytetu Zielonogórskiego, Tom 14]]></dc:source>
<dc:language><![CDATA[pol]]></dc:language>
<dc:language><![CDATA[eng]]></dc:language>
<dc:relation><![CDATA[oai:zbc.uz.zgora.pl:publication:51600]]></dc:relation>
<dc:rights xml:lang="en"><![CDATA[Biblioteka Uniwersytetu Zielonogórskiego]]></dc:rights>
<dc:rights xml:lang="pl"><![CDATA[Biblioteka Uniwersytetu Zielonogórskiego]]></dc:rights>
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