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master's thesis
Mineraloška obilježja pliokvartarnih naslaga i pripadajućih tala prigorja Medvednice
Zagreb: University of Zagreb, Faculty of Science, 2019. urn:nbn:hr:217:374968
Carevski, Filip
University of Zagreb
Faculty of Science
Department of Geology

Institutional repository: Repository of the Faculty of Science

Cite this document

Carevski, F. (2019). Mineraloška obilježja pliokvartarnih naslaga i pripadajućih tala prigorja Medvednice (Master's thesis). Zagreb: University of Zagreb, Faculty of Science. Retrieved from https://urn.nsk.hr/urn:nbn:hr:217:374968

Carevski, Filip. "Mineraloška obilježja pliokvartarnih naslaga i pripadajućih tala prigorja Medvednice." Master's thesis, University of Zagreb, Faculty of Science, 2019. https://urn.nsk.hr/urn:nbn:hr:217:374968

Carevski, Filip. "Mineraloška obilježja pliokvartarnih naslaga i pripadajućih tala prigorja Medvednice." Master's thesis, University of Zagreb, Faculty of Science, 2019. https://urn.nsk.hr/urn:nbn:hr:217:374968

Carevski, F. (2019). 'Mineraloška obilježja pliokvartarnih naslaga i pripadajućih tala prigorja Medvednice', Master's thesis, University of Zagreb, Faculty of Science, accessed 29 April 2024, https://urn.nsk.hr/urn:nbn:hr:217:374968

Carevski F. Mineraloška obilježja pliokvartarnih naslaga i pripadajućih tala prigorja Medvednice [Master's thesis]. Zagreb: University of Zagreb, Faculty of Science; 2019 [cited 2024 April 29] Available at: https://urn.nsk.hr/urn:nbn:hr:217:374968

F. Carevski, "Mineraloška obilježja pliokvartarnih naslaga i pripadajućih tala prigorja Medvednice", Master's thesis, University of Zagreb, Faculty of Science, Zagreb, 2019. Available at: https://urn.nsk.hr/urn:nbn:hr:217:374968

Metadata
TitleMineraloška obilježja pliokvartarnih naslaga i pripadajućih tala prigorja Medvednice
Title (english)Mineralogical properties of plioquaternary deposits and overlaying soils in the southeastern slopes of Medvednica
AuthorFilip Carevski
MentorNenad Tomašić (mentor)
Committee memberNenad Tomašić (predsjednik povjerenstva)
Committee memberMarijan Kovačić (član povjerenstva)
Committee memberĐurđica Pezelj (član povjerenstva)
GranterUniversity of Zagreb
Faculty of Science
(Department of Geology)
Zagreb
Defense date and country2019-02-18, Croatia
Scientific / art field,
discipline and subdiscipline		NATURAL SCIENCES
Geology
Mineralogy and Petrology
Abstract
Ovaj rad se bavi proučavanjem zaglinjenih sedimenata pliokvartarne starosti iz profila s tri lokaliteta jugoistočnog prigorja Medvednice (Horvtovac, Dotrščina, Oporovec). Iz uzoraka su laboratorijskim postupcima za potrebe izrade orijentiranih preparata uklonjeni su organska tvar i Fe-Al-Mn oksidi/oksihidroksidi. Metoda rendgenske difrakcijske analize provedena je na neorijentiranim i orijentiranim preparatima. Neorijentirani preparati pokazali su cjelokupni sastav prije uklanjanja organske tvari i Fe-Al-Mn oksida/oksihidroksida, dok su na orijentiranim preparatima identificirani samo minerali glina na temelju karakterističnih bazalnih maksimuma. U neorijentiranim preparatima određeni su kvarc, muskovit, plagioklas, vermikulit, klorit i kaolinit, a u orijentiranim preparatima utvrđeni su maksimumi smektit-klorita, klorita, dioktaedrijskog vermikulita, illita, dioktaerijskog vermikulit-tinjca, smektita, dioktaedrijskog illita i kaolinit-smektita. Kapacitet kationske izmjene (CEC) mjeren je pomoću bakrovog etilendiaminskog kompleksa na uzorcima prije i nakon uklanjanja prethodno spomenutih faza. Vrijednosti CEC-a su uglavnom veće kod uzoraka s većih dubina zbog nešto većeg postotka bubrećih glina u uzorcima.
Abstract (english)
The aim of this Master’s thesis was to determine mineralogical properties of plioquaternary deposits from the profiles on the three sites of the southeastern slopes of Medvednica (Horvath, Dotrščina, Oporovec). The samples were subjected to laboratory procedures for the purpose of making the orientated preparations, with organic matter and Fe-Al-Mn oxide / oxyhydroxides removed. X-ray diffraction analysis was performed on unoriented and oriented samples. Unoriented preparations showed the entire composition prior to removal of organic matter and Fe-Al-Mn oxide / oxyhydroxide, while clay minerals were identified on the orientated preparations based on the characteristic basal maximum. Quartz, muscovite, plagioclase, vermiculite, chlorite and kaolinite were determined in unoriented preparations, and in the orientated preparations the maximum of smectite-chlorite, chlorite, dioctahedral vermiculite, illite, dioctahedral vermiculite, smectite, dioctahedral illite and kaolinite-smectite were determined. The cation exchange capacity (CEC) was determined using copper ethylenediamine complex and it was measured before and after removal of organic matter and Fe-Al-Mn okside/hidrokside. CEC values a re generally higher in samples of higher depth due to a slightly higher percentage of clay minerals in samples.
Keywords
Keywords (english)
Languagecroatian
URN:NBNurn:nbn:hr:217:374968
Study programmeTitle: Graduate university study of Environmental Geology
Study programme type: university
Study level: graduate
Academic / professional title: magistar/magistra geologije (magistar/magistra geologije)
Type of resourceText
File originBorn digital
Access conditionsOpen access
Terms of useLicence In copyright icon
Created on2019-04-08 09:01:39