izpis_h1_title_alt

Raziskave mobilnosti kovin v solinskem blatu iz Sečoveljskih solin
ID Ramšak, Teja (Author), ID Rogan Šmuc, Nastja (Mentor) More about this mentor... This link opens in a new window, ID Kovač, Nives (Comentor)

.pdfPDF - Presentation file, Download (2,08 MB)
MD5: FAA97689224D2DED07A537CE98429B47
PID: 20.500.12556/rul/cab3cfb3-2a90-4f8a-877e-9c4501febfde

Abstract
Sečoveljske soline so v svetovnem merilu edinstvene. Z aktivno pridelavo soli na petoli veljajo za območje, kjer je bilo izvedeno veliko raziskav flore in favne, le malo raziskav pa je bilo namenjeno študiju in aplikativni uporabi solinskega blata. V splošnem imajo vzorci solinskega blata (iz različnih lokacij/vzorčnih mest) zelo podobno mineralno in geokemično sestavo, kar nakazuje na širšo potencialno možnost zajema solinskega blata kot vhodne surovine za balneoterapevtske namene. Za razumevanje celotnega sistema ionske izmenjave med tekočo in trdno fazo smo v magistrskem delu raziskali variabilnosti elementne sestave solinskega blata, slanice in porne vode blata, ki predstavljajo pomembne lastnosti za terapevtsko uporabo peloidov. Pri tem imajo seveda glavno vlogo težke kovine in polkovine ter sledne prvine, ki so prisotne v solinskem blatu in slanici ter imajo zmožnost njihovega izluževanja pri uporabi blata za balneoterapevtske oz. peloterapevske namene. Rezultati so pokazali, da slanost in zorenje blata ne vplivata na mineralno sestavo trdne faze. Vplivata na mobilnost kovin, saj se pri najvišji slanosti slanice (27,5 Bé=27,2 S %), ki jo dosežejo Sečoveljske soline v poletni sezoni, vsebnost težkih kovin in polkovin ter sledne prvine v solinskem blatu zmanjšajo in zato povečajo v vodni fazi. Cr v trdni fazi iz 112 mg kg-1 pade na 93 mg kg-1 ob koncu eksperimenta (tk), prav tako Ni iz 77,3 mg kg-1 pade na 68,3 mg kg-1 ob tk. Izračunani faktor obogatitve (EF) je bil pri elementih Ba, Mn in Sr pod vrednostjo 1, kar pomeni, da solinsko blato ni obogateno s temi tremi elementi. Pri elementih As, Co, Cr, Cu, Ni, Pb, Zn so bile vrednosti faktorja obogatitve povsod nižje od 3, kar pomeni, da ima solinsko blato manjšo obogatitev z navedenimi elementi.

Language:Slovenian
Keywords:Sečoveljske soline, mobilnost težkih kovin, solinsko blato, slanica, laboratorijski eksperiment
Work type:Bachelor thesis/paper
Organization:NTF - Faculty of Natural Sciences and Engineering
Year:2017
PID:20.500.12556/RUL-96522 This link opens in a new window
COBISS.SI-ID:1358430 This link opens in a new window
Publication date in RUL:04.10.2017
Views:1934
Downloads:698
Metadata:XML DC-XML DC-RDF
:
Copy citation
Share:Bookmark and Share

Secondary language

Language:English
Title:Metal mobility research in saline mud from Sečovlje salina
Abstract:
Sečovlje Salina is in worldwide unique places. Saline sediment (saline healing mud or “fango”) from the Sečovlje Salina is traditionally used in the coastal health resorts as a virgin material for medical treatment, wellness and relax purposes. Therapeutic qualities of the healing mud depends on its mineralogical composition and physical, mineralogical, geochemical and biological properties. Their microbial and potentially toxic elements contamination are the most important features affecting user safety. However, the degree of metal toxicity (and its regulation) for natural healing mud is still under discussion. Therefore, the influence of the overlying water salinity on the mobility of heavy metals (and some other geochemical characteristics) was studied for saline sediment of the Sečovlje Salina. Experiments takes place in eight tanks under defined conditions i.e. at day (21 °C): night (16 °C) cycle for three months. Sediment, sampled in Sečovlje Salina, was covered with water of different salinities and mixed/stirred every week during the experimental period. Salinity and maturation of sediment does not significantly affect its mineral composition. In the water phase, concentrations of most elements (As, Ba, Cu, Mo, Mn, Ni, Sr, Sb) rise from the beginning to the end of the experiment, whereas the heavy metals (potentially toxic elements) decreasing trend in sediment was observed at that time. Enrichment factor (EF) was under 1 value for Ba, Sr, Mn, which means that the salt mud is not enriched with stated elements. Elements Co, Cr, Cu, Ni, Pb, Zn had EF value under 3, which means that sediments have small enrichment with these elements.

Keywords:Sečovlje Salina, elements mobility, saline sediment, brine, laboratory experiment

Similar documents

Similar works from RUL:
Similar works from other Slovenian collections:

Back