Chemical and mineralogical characteristics of peloids in Turkey

Abstract To investigate the physical, chemical, and mineralogical characteristics of peloids, which are being used traditionally and historically across Turkey, and evaluate their suitability and potential for use in peloidotherapy. Five peloid samples were gathered from their places of origin, namely Gölemezli, Dalyan, Köprüköy, Gökçeada, and Dikili. Mineral analysis and physical and chemical analyses including electrical conductivity, density, cations, anions, trace elements, organic matters, and water retention capacity at 105 °C were performed. The peloids contained a combination of clay minerals (mainly montmorillonite, kaolinite, and muscovite) and non-clay minerals (mainly quartz, calcite, dolomite, and albite) except for Gölemezli peloid, which was dominated by calcite. The other minerals (i.e., chloride-serpentine, sphalerite, pyrite, magnesium calcite, cristobalite) were also found in some peloids. Gölemezli, Dalyan, and Köprüköy peloids had high total organic matters, mainly humic substances. The water retention capacity was high in Dalyan, Köprüköy, and Dikili peloids. All peloids had a pH value slightly greater than 7 (range 7.93–8.69). Dalyan, Köprüköy, and Dikili peloids had a high water retention capacity. Dalyan and Gökçeada peloids had a high electrical conductivity, 22.040 and 9.020 μS/cm, respectively. The density of peloids was ranged between 1.240 (Gölemezli) and 1.450 (Gökçeada) g/$ cm^{3} $. Total mineralization of investigated peloids was greater than 1000 mg/L: Köprüköy, 2754.8 mg/L; Gölemezli, 3092.8 mg/L; Dikili, 4044.6 mg/L; Gökçeada, 6576.6 mg/L; and Dalyan, 11782.9 mg/L, mainly sodium, magnesium, calcium, chloride, sulfate, bicarbonate, and metasilicic acid. The levels of trace elements were low (≤ 2.0 mg/L) in all peloids. The peloids contained various amounts of clay minerals (mainly montmorillonite, kaolinite, and muscovite), non-clay minerals (mainly quartz, calcite, dolomite, and albite), organic matters (mainly humic acid), cations (mainly sodium, magnesium, and calcium), anions (mainly chloride, sulfate, and bicarbonate), and insoluble compounds (mainly metasilicic acid). The physical, chemical, and mineralogical properties of peloids suggest their suitability and potential for use in peloidotherapeutic applications. Ausführliche Beschreibung

Gespeichert in:

Autor*in:	Özay, Pelin [verfasserIn] Karagülle, Mine [verfasserIn] Kardeş, Sinan [verfasserIn] Karagülle, Müfit Zeki [verfasserIn]

Format:	E-Artikel
Sprache:	Englisch

Erschienen:	2020

Schlagwörter:	Turkey peloids Muds Peloidotherapy Mud therapy Clay

Übergeordnetes Werk:	Enthalten in: Environmental monitoring and assessment - Dordrecht [u.a.] : Springer Science + Business Media B.V, 1981, 192(2020), 12 vom: Dez.
Übergeordnetes Werk:	volume:192 ; year:2020 ; number:12 ; month:12

Links:	Volltext

DOI / URN:	10.1007/s10661-020-08777-2

Katalog-ID:	SPR042235502

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520			\|a Abstract To investigate the physical, chemical, and mineralogical characteristics of peloids, which are being used traditionally and historically across Turkey, and evaluate their suitability and potential for use in peloidotherapy. Five peloid samples were gathered from their places of origin, namely Gölemezli, Dalyan, Köprüköy, Gökçeada, and Dikili. Mineral analysis and physical and chemical analyses including electrical conductivity, density, cations, anions, trace elements, organic matters, and water retention capacity at 105 °C were performed. The peloids contained a combination of clay minerals (mainly montmorillonite, kaolinite, and muscovite) and non-clay minerals (mainly quartz, calcite, dolomite, and albite) except for Gölemezli peloid, which was dominated by calcite. The other minerals (i.e., chloride-serpentine, sphalerite, pyrite, magnesium calcite, cristobalite) were also found in some peloids. Gölemezli, Dalyan, and Köprüköy peloids had high total organic matters, mainly humic substances. The water retention capacity was high in Dalyan, Köprüköy, and Dikili peloids. All peloids had a pH value slightly greater than 7 (range 7.93–8.69). Dalyan, Köprüköy, and Dikili peloids had a high water retention capacity. Dalyan and Gökçeada peloids had a high electrical conductivity, 22.040 and 9.020 μS/cm, respectively. The density of peloids was ranged between 1.240 (Gölemezli) and 1.450 (Gökçeada) g/$ cm^{3} $. Total mineralization of investigated peloids was greater than 1000 mg/L: Köprüköy, 2754.8 mg/L; Gölemezli, 3092.8 mg/L; Dikili, 4044.6 mg/L; Gökçeada, 6576.6 mg/L; and Dalyan, 11782.9 mg/L, mainly sodium, magnesium, calcium, chloride, sulfate, bicarbonate, and metasilicic acid. The levels of trace elements were low (≤ 2.0 mg/L) in all peloids. The peloids contained various amounts of clay minerals (mainly montmorillonite, kaolinite, and muscovite), non-clay minerals (mainly quartz, calcite, dolomite, and albite), organic matters (mainly humic acid), cations (mainly sodium, magnesium, and calcium), anions (mainly chloride, sulfate, and bicarbonate), and insoluble compounds (mainly metasilicic acid). The physical, chemical, and mineralogical properties of peloids suggest their suitability and potential for use in peloidotherapeutic applications.
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Indexfelder

author_variant	p ö pö m k mk s k sk m z k mz mzk
matchkey_str	article:15732959:2020----::hmclnmnrlgclhrceitcop
hierarchy_sort_str	2020
bklnumber	30.00 43.00
publishDate	2020
allfields	10.1007/s10661-020-08777-2 doi (DE-627)SPR042235502 (DE-599)SPRs10661-020-08777-2-e (SPR)s10661-020-08777-2-e DE-627 ger DE-627 rakwb eng 333.7 ASE 30.00 bkl 43.00 bkl Özay, Pelin verfasserin aut Chemical and mineralogical characteristics of peloids in Turkey 2020 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier Abstract To investigate the physical, chemical, and mineralogical characteristics of peloids, which are being used traditionally and historically across Turkey, and evaluate their suitability and potential for use in peloidotherapy. Five peloid samples were gathered from their places of origin, namely Gölemezli, Dalyan, Köprüköy, Gökçeada, and Dikili. Mineral analysis and physical and chemical analyses including electrical conductivity, density, cations, anions, trace elements, organic matters, and water retention capacity at 105 °C were performed. The peloids contained a combination of clay minerals (mainly montmorillonite, kaolinite, and muscovite) and non-clay minerals (mainly quartz, calcite, dolomite, and albite) except for Gölemezli peloid, which was dominated by calcite. The other minerals (i.e., chloride-serpentine, sphalerite, pyrite, magnesium calcite, cristobalite) were also found in some peloids. Gölemezli, Dalyan, and Köprüköy peloids had high total organic matters, mainly humic substances. The water retention capacity was high in Dalyan, Köprüköy, and Dikili peloids. All peloids had a pH value slightly greater than 7 (range 7.93–8.69). Dalyan, Köprüköy, and Dikili peloids had a high water retention capacity. Dalyan and Gökçeada peloids had a high electrical conductivity, 22.040 and 9.020 μS/cm, respectively. The density of peloids was ranged between 1.240 (Gölemezli) and 1.450 (Gökçeada) g/$ cm^{3} $. Total mineralization of investigated peloids was greater than 1000 mg/L: Köprüköy, 2754.8 mg/L; Gölemezli, 3092.8 mg/L; Dikili, 4044.6 mg/L; Gökçeada, 6576.6 mg/L; and Dalyan, 11782.9 mg/L, mainly sodium, magnesium, calcium, chloride, sulfate, bicarbonate, and metasilicic acid. The levels of trace elements were low (≤ 2.0 mg/L) in all peloids. The peloids contained various amounts of clay minerals (mainly montmorillonite, kaolinite, and muscovite), non-clay minerals (mainly quartz, calcite, dolomite, and albite), organic matters (mainly humic acid), cations (mainly sodium, magnesium, and calcium), anions (mainly chloride, sulfate, and bicarbonate), and insoluble compounds (mainly metasilicic acid). The physical, chemical, and mineralogical properties of peloids suggest their suitability and potential for use in peloidotherapeutic applications. Turkey peloids (dpeaa)DE-He213 Muds (dpeaa)DE-He213 Peloidotherapy (dpeaa)DE-He213 Mud therapy (dpeaa)DE-He213 Clay (dpeaa)DE-He213 Karagülle, Mine verfasserin aut Kardeş, Sinan verfasserin aut Karagülle, Müfit Zeki verfasserin aut Enthalten in Environmental monitoring and assessment Dordrecht [u.a.] : Springer Science + Business Media B.V, 1981 192(2020), 12 vom: Dez. (DE-627)31281738X (DE-600)2012242-1 1573-2959 nnns volume:192 year:2020 number:12 month:12 https://dx.doi.org/10.1007/s10661-020-08777-2 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER SSG-OPC-GGO SSG-OPC-ASE GBV_ILN_11 GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_32 GBV_ILN_39 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_74 GBV_ILN_90 GBV_ILN_95 GBV_ILN_100 GBV_ILN_105 GBV_ILN_110 GBV_ILN_120 GBV_ILN_138 GBV_ILN_150 GBV_ILN_151 GBV_ILN_152 GBV_ILN_161 GBV_ILN_170 GBV_ILN_171 GBV_ILN_187 GBV_ILN_213 GBV_ILN_224 GBV_ILN_230 GBV_ILN_250 GBV_ILN_281 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_602 GBV_ILN_636 GBV_ILN_702 GBV_ILN_2001 GBV_ILN_2003 GBV_ILN_2004 GBV_ILN_2005 GBV_ILN_2006 GBV_ILN_2007 GBV_ILN_2008 GBV_ILN_2009 GBV_ILN_2010 GBV_ILN_2011 GBV_ILN_2014 GBV_ILN_2015 GBV_ILN_2020 GBV_ILN_2021 GBV_ILN_2025 GBV_ILN_2026 GBV_ILN_2027 GBV_ILN_2031 GBV_ILN_2034 GBV_ILN_2037 GBV_ILN_2038 GBV_ILN_2039 GBV_ILN_2044 GBV_ILN_2048 GBV_ILN_2049 GBV_ILN_2050 GBV_ILN_2055 GBV_ILN_2056 GBV_ILN_2057 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 GBV_ILN_2088 GBV_ILN_2093 GBV_ILN_2106 GBV_ILN_2107 GBV_ILN_2108 GBV_ILN_2110 GBV_ILN_2111 GBV_ILN_2112 GBV_ILN_2113 GBV_ILN_2118 GBV_ILN_2122 GBV_ILN_2129 GBV_ILN_2143 GBV_ILN_2144 GBV_ILN_2147 GBV_ILN_2148 GBV_ILN_2152 GBV_ILN_2153 GBV_ILN_2188 GBV_ILN_2190 GBV_ILN_2232 GBV_ILN_2336 GBV_ILN_2446 GBV_ILN_2470 GBV_ILN_2472 GBV_ILN_2507 GBV_ILN_2522 GBV_ILN_2548 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4046 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4242 GBV_ILN_4246 GBV_ILN_4249 GBV_ILN_4251 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4313 GBV_ILN_4322 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4326 GBV_ILN_4328 GBV_ILN_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4336 GBV_ILN_4338 GBV_ILN_4393 GBV_ILN_4700 30.00 ASE 43.00 ASE AR 192 2020 12 12
spelling	10.1007/s10661-020-08777-2 doi (DE-627)SPR042235502 (DE-599)SPRs10661-020-08777-2-e (SPR)s10661-020-08777-2-e DE-627 ger DE-627 rakwb eng 333.7 ASE 30.00 bkl 43.00 bkl Özay, Pelin verfasserin aut Chemical and mineralogical characteristics of peloids in Turkey 2020 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier Abstract To investigate the physical, chemical, and mineralogical characteristics of peloids, which are being used traditionally and historically across Turkey, and evaluate their suitability and potential for use in peloidotherapy. Five peloid samples were gathered from their places of origin, namely Gölemezli, Dalyan, Köprüköy, Gökçeada, and Dikili. Mineral analysis and physical and chemical analyses including electrical conductivity, density, cations, anions, trace elements, organic matters, and water retention capacity at 105 °C were performed. The peloids contained a combination of clay minerals (mainly montmorillonite, kaolinite, and muscovite) and non-clay minerals (mainly quartz, calcite, dolomite, and albite) except for Gölemezli peloid, which was dominated by calcite. The other minerals (i.e., chloride-serpentine, sphalerite, pyrite, magnesium calcite, cristobalite) were also found in some peloids. Gölemezli, Dalyan, and Köprüköy peloids had high total organic matters, mainly humic substances. The water retention capacity was high in Dalyan, Köprüköy, and Dikili peloids. All peloids had a pH value slightly greater than 7 (range 7.93–8.69). Dalyan, Köprüköy, and Dikili peloids had a high water retention capacity. Dalyan and Gökçeada peloids had a high electrical conductivity, 22.040 and 9.020 μS/cm, respectively. The density of peloids was ranged between 1.240 (Gölemezli) and 1.450 (Gökçeada) g/$ cm^{3} $. Total mineralization of investigated peloids was greater than 1000 mg/L: Köprüköy, 2754.8 mg/L; Gölemezli, 3092.8 mg/L; Dikili, 4044.6 mg/L; Gökçeada, 6576.6 mg/L; and Dalyan, 11782.9 mg/L, mainly sodium, magnesium, calcium, chloride, sulfate, bicarbonate, and metasilicic acid. The levels of trace elements were low (≤ 2.0 mg/L) in all peloids. The peloids contained various amounts of clay minerals (mainly montmorillonite, kaolinite, and muscovite), non-clay minerals (mainly quartz, calcite, dolomite, and albite), organic matters (mainly humic acid), cations (mainly sodium, magnesium, and calcium), anions (mainly chloride, sulfate, and bicarbonate), and insoluble compounds (mainly metasilicic acid). The physical, chemical, and mineralogical properties of peloids suggest their suitability and potential for use in peloidotherapeutic applications. Turkey peloids (dpeaa)DE-He213 Muds (dpeaa)DE-He213 Peloidotherapy (dpeaa)DE-He213 Mud therapy (dpeaa)DE-He213 Clay (dpeaa)DE-He213 Karagülle, Mine verfasserin aut Kardeş, Sinan verfasserin aut Karagülle, Müfit Zeki verfasserin aut Enthalten in Environmental monitoring and assessment Dordrecht [u.a.] : Springer Science + Business Media B.V, 1981 192(2020), 12 vom: Dez. (DE-627)31281738X (DE-600)2012242-1 1573-2959 nnns volume:192 year:2020 number:12 month:12 https://dx.doi.org/10.1007/s10661-020-08777-2 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER SSG-OPC-GGO SSG-OPC-ASE GBV_ILN_11 GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_32 GBV_ILN_39 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_74 GBV_ILN_90 GBV_ILN_95 GBV_ILN_100 GBV_ILN_105 GBV_ILN_110 GBV_ILN_120 GBV_ILN_138 GBV_ILN_150 GBV_ILN_151 GBV_ILN_152 GBV_ILN_161 GBV_ILN_170 GBV_ILN_171 GBV_ILN_187 GBV_ILN_213 GBV_ILN_224 GBV_ILN_230 GBV_ILN_250 GBV_ILN_281 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_602 GBV_ILN_636 GBV_ILN_702 GBV_ILN_2001 GBV_ILN_2003 GBV_ILN_2004 GBV_ILN_2005 GBV_ILN_2006 GBV_ILN_2007 GBV_ILN_2008 GBV_ILN_2009 GBV_ILN_2010 GBV_ILN_2011 GBV_ILN_2014 GBV_ILN_2015 GBV_ILN_2020 GBV_ILN_2021 GBV_ILN_2025 GBV_ILN_2026 GBV_ILN_2027 GBV_ILN_2031 GBV_ILN_2034 GBV_ILN_2037 GBV_ILN_2038 GBV_ILN_2039 GBV_ILN_2044 GBV_ILN_2048 GBV_ILN_2049 GBV_ILN_2050 GBV_ILN_2055 GBV_ILN_2056 GBV_ILN_2057 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 GBV_ILN_2088 GBV_ILN_2093 GBV_ILN_2106 GBV_ILN_2107 GBV_ILN_2108 GBV_ILN_2110 GBV_ILN_2111 GBV_ILN_2112 GBV_ILN_2113 GBV_ILN_2118 GBV_ILN_2122 GBV_ILN_2129 GBV_ILN_2143 GBV_ILN_2144 GBV_ILN_2147 GBV_ILN_2148 GBV_ILN_2152 GBV_ILN_2153 GBV_ILN_2188 GBV_ILN_2190 GBV_ILN_2232 GBV_ILN_2336 GBV_ILN_2446 GBV_ILN_2470 GBV_ILN_2472 GBV_ILN_2507 GBV_ILN_2522 GBV_ILN_2548 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4046 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4242 GBV_ILN_4246 GBV_ILN_4249 GBV_ILN_4251 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4313 GBV_ILN_4322 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4326 GBV_ILN_4328 GBV_ILN_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4336 GBV_ILN_4338 GBV_ILN_4393 GBV_ILN_4700 30.00 ASE 43.00 ASE AR 192 2020 12 12
allfields_unstemmed	10.1007/s10661-020-08777-2 doi (DE-627)SPR042235502 (DE-599)SPRs10661-020-08777-2-e (SPR)s10661-020-08777-2-e DE-627 ger DE-627 rakwb eng 333.7 ASE 30.00 bkl 43.00 bkl Özay, Pelin verfasserin aut Chemical and mineralogical characteristics of peloids in Turkey 2020 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier Abstract To investigate the physical, chemical, and mineralogical characteristics of peloids, which are being used traditionally and historically across Turkey, and evaluate their suitability and potential for use in peloidotherapy. Five peloid samples were gathered from their places of origin, namely Gölemezli, Dalyan, Köprüköy, Gökçeada, and Dikili. Mineral analysis and physical and chemical analyses including electrical conductivity, density, cations, anions, trace elements, organic matters, and water retention capacity at 105 °C were performed. The peloids contained a combination of clay minerals (mainly montmorillonite, kaolinite, and muscovite) and non-clay minerals (mainly quartz, calcite, dolomite, and albite) except for Gölemezli peloid, which was dominated by calcite. The other minerals (i.e., chloride-serpentine, sphalerite, pyrite, magnesium calcite, cristobalite) were also found in some peloids. Gölemezli, Dalyan, and Köprüköy peloids had high total organic matters, mainly humic substances. The water retention capacity was high in Dalyan, Köprüköy, and Dikili peloids. All peloids had a pH value slightly greater than 7 (range 7.93–8.69). Dalyan, Köprüköy, and Dikili peloids had a high water retention capacity. Dalyan and Gökçeada peloids had a high electrical conductivity, 22.040 and 9.020 μS/cm, respectively. The density of peloids was ranged between 1.240 (Gölemezli) and 1.450 (Gökçeada) g/$ cm^{3} $. Total mineralization of investigated peloids was greater than 1000 mg/L: Köprüköy, 2754.8 mg/L; Gölemezli, 3092.8 mg/L; Dikili, 4044.6 mg/L; Gökçeada, 6576.6 mg/L; and Dalyan, 11782.9 mg/L, mainly sodium, magnesium, calcium, chloride, sulfate, bicarbonate, and metasilicic acid. The levels of trace elements were low (≤ 2.0 mg/L) in all peloids. The peloids contained various amounts of clay minerals (mainly montmorillonite, kaolinite, and muscovite), non-clay minerals (mainly quartz, calcite, dolomite, and albite), organic matters (mainly humic acid), cations (mainly sodium, magnesium, and calcium), anions (mainly chloride, sulfate, and bicarbonate), and insoluble compounds (mainly metasilicic acid). The physical, chemical, and mineralogical properties of peloids suggest their suitability and potential for use in peloidotherapeutic applications. Turkey peloids (dpeaa)DE-He213 Muds (dpeaa)DE-He213 Peloidotherapy (dpeaa)DE-He213 Mud therapy (dpeaa)DE-He213 Clay (dpeaa)DE-He213 Karagülle, Mine verfasserin aut Kardeş, Sinan verfasserin aut Karagülle, Müfit Zeki verfasserin aut Enthalten in Environmental monitoring and assessment Dordrecht [u.a.] : Springer Science + Business Media B.V, 1981 192(2020), 12 vom: Dez. (DE-627)31281738X (DE-600)2012242-1 1573-2959 nnns volume:192 year:2020 number:12 month:12 https://dx.doi.org/10.1007/s10661-020-08777-2 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER SSG-OPC-GGO SSG-OPC-ASE GBV_ILN_11 GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_32 GBV_ILN_39 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_74 GBV_ILN_90 GBV_ILN_95 GBV_ILN_100 GBV_ILN_105 GBV_ILN_110 GBV_ILN_120 GBV_ILN_138 GBV_ILN_150 GBV_ILN_151 GBV_ILN_152 GBV_ILN_161 GBV_ILN_170 GBV_ILN_171 GBV_ILN_187 GBV_ILN_213 GBV_ILN_224 GBV_ILN_230 GBV_ILN_250 GBV_ILN_281 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_602 GBV_ILN_636 GBV_ILN_702 GBV_ILN_2001 GBV_ILN_2003 GBV_ILN_2004 GBV_ILN_2005 GBV_ILN_2006 GBV_ILN_2007 GBV_ILN_2008 GBV_ILN_2009 GBV_ILN_2010 GBV_ILN_2011 GBV_ILN_2014 GBV_ILN_2015 GBV_ILN_2020 GBV_ILN_2021 GBV_ILN_2025 GBV_ILN_2026 GBV_ILN_2027 GBV_ILN_2031 GBV_ILN_2034 GBV_ILN_2037 GBV_ILN_2038 GBV_ILN_2039 GBV_ILN_2044 GBV_ILN_2048 GBV_ILN_2049 GBV_ILN_2050 GBV_ILN_2055 GBV_ILN_2056 GBV_ILN_2057 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 GBV_ILN_2088 GBV_ILN_2093 GBV_ILN_2106 GBV_ILN_2107 GBV_ILN_2108 GBV_ILN_2110 GBV_ILN_2111 GBV_ILN_2112 GBV_ILN_2113 GBV_ILN_2118 GBV_ILN_2122 GBV_ILN_2129 GBV_ILN_2143 GBV_ILN_2144 GBV_ILN_2147 GBV_ILN_2148 GBV_ILN_2152 GBV_ILN_2153 GBV_ILN_2188 GBV_ILN_2190 GBV_ILN_2232 GBV_ILN_2336 GBV_ILN_2446 GBV_ILN_2470 GBV_ILN_2472 GBV_ILN_2507 GBV_ILN_2522 GBV_ILN_2548 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4046 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4242 GBV_ILN_4246 GBV_ILN_4249 GBV_ILN_4251 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4313 GBV_ILN_4322 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4326 GBV_ILN_4328 GBV_ILN_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4336 GBV_ILN_4338 GBV_ILN_4393 GBV_ILN_4700 30.00 ASE 43.00 ASE AR 192 2020 12 12
allfieldsGer	10.1007/s10661-020-08777-2 doi (DE-627)SPR042235502 (DE-599)SPRs10661-020-08777-2-e (SPR)s10661-020-08777-2-e DE-627 ger DE-627 rakwb eng 333.7 ASE 30.00 bkl 43.00 bkl Özay, Pelin verfasserin aut Chemical and mineralogical characteristics of peloids in Turkey 2020 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier Abstract To investigate the physical, chemical, and mineralogical characteristics of peloids, which are being used traditionally and historically across Turkey, and evaluate their suitability and potential for use in peloidotherapy. Five peloid samples were gathered from their places of origin, namely Gölemezli, Dalyan, Köprüköy, Gökçeada, and Dikili. Mineral analysis and physical and chemical analyses including electrical conductivity, density, cations, anions, trace elements, organic matters, and water retention capacity at 105 °C were performed. The peloids contained a combination of clay minerals (mainly montmorillonite, kaolinite, and muscovite) and non-clay minerals (mainly quartz, calcite, dolomite, and albite) except for Gölemezli peloid, which was dominated by calcite. The other minerals (i.e., chloride-serpentine, sphalerite, pyrite, magnesium calcite, cristobalite) were also found in some peloids. Gölemezli, Dalyan, and Köprüköy peloids had high total organic matters, mainly humic substances. The water retention capacity was high in Dalyan, Köprüköy, and Dikili peloids. All peloids had a pH value slightly greater than 7 (range 7.93–8.69). Dalyan, Köprüköy, and Dikili peloids had a high water retention capacity. Dalyan and Gökçeada peloids had a high electrical conductivity, 22.040 and 9.020 μS/cm, respectively. The density of peloids was ranged between 1.240 (Gölemezli) and 1.450 (Gökçeada) g/$ cm^{3} $. Total mineralization of investigated peloids was greater than 1000 mg/L: Köprüköy, 2754.8 mg/L; Gölemezli, 3092.8 mg/L; Dikili, 4044.6 mg/L; Gökçeada, 6576.6 mg/L; and Dalyan, 11782.9 mg/L, mainly sodium, magnesium, calcium, chloride, sulfate, bicarbonate, and metasilicic acid. The levels of trace elements were low (≤ 2.0 mg/L) in all peloids. The peloids contained various amounts of clay minerals (mainly montmorillonite, kaolinite, and muscovite), non-clay minerals (mainly quartz, calcite, dolomite, and albite), organic matters (mainly humic acid), cations (mainly sodium, magnesium, and calcium), anions (mainly chloride, sulfate, and bicarbonate), and insoluble compounds (mainly metasilicic acid). The physical, chemical, and mineralogical properties of peloids suggest their suitability and potential for use in peloidotherapeutic applications. Turkey peloids (dpeaa)DE-He213 Muds (dpeaa)DE-He213 Peloidotherapy (dpeaa)DE-He213 Mud therapy (dpeaa)DE-He213 Clay (dpeaa)DE-He213 Karagülle, Mine verfasserin aut Kardeş, Sinan verfasserin aut Karagülle, Müfit Zeki verfasserin aut Enthalten in Environmental monitoring and assessment Dordrecht [u.a.] : Springer Science + Business Media B.V, 1981 192(2020), 12 vom: Dez. (DE-627)31281738X (DE-600)2012242-1 1573-2959 nnns volume:192 year:2020 number:12 month:12 https://dx.doi.org/10.1007/s10661-020-08777-2 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER SSG-OPC-GGO SSG-OPC-ASE GBV_ILN_11 GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_32 GBV_ILN_39 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_74 GBV_ILN_90 GBV_ILN_95 GBV_ILN_100 GBV_ILN_105 GBV_ILN_110 GBV_ILN_120 GBV_ILN_138 GBV_ILN_150 GBV_ILN_151 GBV_ILN_152 GBV_ILN_161 GBV_ILN_170 GBV_ILN_171 GBV_ILN_187 GBV_ILN_213 GBV_ILN_224 GBV_ILN_230 GBV_ILN_250 GBV_ILN_281 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_602 GBV_ILN_636 GBV_ILN_702 GBV_ILN_2001 GBV_ILN_2003 GBV_ILN_2004 GBV_ILN_2005 GBV_ILN_2006 GBV_ILN_2007 GBV_ILN_2008 GBV_ILN_2009 GBV_ILN_2010 GBV_ILN_2011 GBV_ILN_2014 GBV_ILN_2015 GBV_ILN_2020 GBV_ILN_2021 GBV_ILN_2025 GBV_ILN_2026 GBV_ILN_2027 GBV_ILN_2031 GBV_ILN_2034 GBV_ILN_2037 GBV_ILN_2038 GBV_ILN_2039 GBV_ILN_2044 GBV_ILN_2048 GBV_ILN_2049 GBV_ILN_2050 GBV_ILN_2055 GBV_ILN_2056 GBV_ILN_2057 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 GBV_ILN_2088 GBV_ILN_2093 GBV_ILN_2106 GBV_ILN_2107 GBV_ILN_2108 GBV_ILN_2110 GBV_ILN_2111 GBV_ILN_2112 GBV_ILN_2113 GBV_ILN_2118 GBV_ILN_2122 GBV_ILN_2129 GBV_ILN_2143 GBV_ILN_2144 GBV_ILN_2147 GBV_ILN_2148 GBV_ILN_2152 GBV_ILN_2153 GBV_ILN_2188 GBV_ILN_2190 GBV_ILN_2232 GBV_ILN_2336 GBV_ILN_2446 GBV_ILN_2470 GBV_ILN_2472 GBV_ILN_2507 GBV_ILN_2522 GBV_ILN_2548 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4046 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4242 GBV_ILN_4246 GBV_ILN_4249 GBV_ILN_4251 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4313 GBV_ILN_4322 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4326 GBV_ILN_4328 GBV_ILN_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4336 GBV_ILN_4338 GBV_ILN_4393 GBV_ILN_4700 30.00 ASE 43.00 ASE AR 192 2020 12 12
allfieldsSound	10.1007/s10661-020-08777-2 doi (DE-627)SPR042235502 (DE-599)SPRs10661-020-08777-2-e (SPR)s10661-020-08777-2-e DE-627 ger DE-627 rakwb eng 333.7 ASE 30.00 bkl 43.00 bkl Özay, Pelin verfasserin aut Chemical and mineralogical characteristics of peloids in Turkey 2020 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier Abstract To investigate the physical, chemical, and mineralogical characteristics of peloids, which are being used traditionally and historically across Turkey, and evaluate their suitability and potential for use in peloidotherapy. Five peloid samples were gathered from their places of origin, namely Gölemezli, Dalyan, Köprüköy, Gökçeada, and Dikili. Mineral analysis and physical and chemical analyses including electrical conductivity, density, cations, anions, trace elements, organic matters, and water retention capacity at 105 °C were performed. The peloids contained a combination of clay minerals (mainly montmorillonite, kaolinite, and muscovite) and non-clay minerals (mainly quartz, calcite, dolomite, and albite) except for Gölemezli peloid, which was dominated by calcite. The other minerals (i.e., chloride-serpentine, sphalerite, pyrite, magnesium calcite, cristobalite) were also found in some peloids. Gölemezli, Dalyan, and Köprüköy peloids had high total organic matters, mainly humic substances. The water retention capacity was high in Dalyan, Köprüköy, and Dikili peloids. All peloids had a pH value slightly greater than 7 (range 7.93–8.69). Dalyan, Köprüköy, and Dikili peloids had a high water retention capacity. Dalyan and Gökçeada peloids had a high electrical conductivity, 22.040 and 9.020 μS/cm, respectively. The density of peloids was ranged between 1.240 (Gölemezli) and 1.450 (Gökçeada) g/$ cm^{3} $. Total mineralization of investigated peloids was greater than 1000 mg/L: Köprüköy, 2754.8 mg/L; Gölemezli, 3092.8 mg/L; Dikili, 4044.6 mg/L; Gökçeada, 6576.6 mg/L; and Dalyan, 11782.9 mg/L, mainly sodium, magnesium, calcium, chloride, sulfate, bicarbonate, and metasilicic acid. The levels of trace elements were low (≤ 2.0 mg/L) in all peloids. The peloids contained various amounts of clay minerals (mainly montmorillonite, kaolinite, and muscovite), non-clay minerals (mainly quartz, calcite, dolomite, and albite), organic matters (mainly humic acid), cations (mainly sodium, magnesium, and calcium), anions (mainly chloride, sulfate, and bicarbonate), and insoluble compounds (mainly metasilicic acid). The physical, chemical, and mineralogical properties of peloids suggest their suitability and potential for use in peloidotherapeutic applications. Turkey peloids (dpeaa)DE-He213 Muds (dpeaa)DE-He213 Peloidotherapy (dpeaa)DE-He213 Mud therapy (dpeaa)DE-He213 Clay (dpeaa)DE-He213 Karagülle, Mine verfasserin aut Kardeş, Sinan verfasserin aut Karagülle, Müfit Zeki verfasserin aut Enthalten in Environmental monitoring and assessment Dordrecht [u.a.] : Springer Science + Business Media B.V, 1981 192(2020), 12 vom: Dez. (DE-627)31281738X (DE-600)2012242-1 1573-2959 nnns volume:192 year:2020 number:12 month:12 https://dx.doi.org/10.1007/s10661-020-08777-2 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER SSG-OPC-GGO SSG-OPC-ASE GBV_ILN_11 GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_32 GBV_ILN_39 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_74 GBV_ILN_90 GBV_ILN_95 GBV_ILN_100 GBV_ILN_105 GBV_ILN_110 GBV_ILN_120 GBV_ILN_138 GBV_ILN_150 GBV_ILN_151 GBV_ILN_152 GBV_ILN_161 GBV_ILN_170 GBV_ILN_171 GBV_ILN_187 GBV_ILN_213 GBV_ILN_224 GBV_ILN_230 GBV_ILN_250 GBV_ILN_281 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_602 GBV_ILN_636 GBV_ILN_702 GBV_ILN_2001 GBV_ILN_2003 GBV_ILN_2004 GBV_ILN_2005 GBV_ILN_2006 GBV_ILN_2007 GBV_ILN_2008 GBV_ILN_2009 GBV_ILN_2010 GBV_ILN_2011 GBV_ILN_2014 GBV_ILN_2015 GBV_ILN_2020 GBV_ILN_2021 GBV_ILN_2025 GBV_ILN_2026 GBV_ILN_2027 GBV_ILN_2031 GBV_ILN_2034 GBV_ILN_2037 GBV_ILN_2038 GBV_ILN_2039 GBV_ILN_2044 GBV_ILN_2048 GBV_ILN_2049 GBV_ILN_2050 GBV_ILN_2055 GBV_ILN_2056 GBV_ILN_2057 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 GBV_ILN_2088 GBV_ILN_2093 GBV_ILN_2106 GBV_ILN_2107 GBV_ILN_2108 GBV_ILN_2110 GBV_ILN_2111 GBV_ILN_2112 GBV_ILN_2113 GBV_ILN_2118 GBV_ILN_2122 GBV_ILN_2129 GBV_ILN_2143 GBV_ILN_2144 GBV_ILN_2147 GBV_ILN_2148 GBV_ILN_2152 GBV_ILN_2153 GBV_ILN_2188 GBV_ILN_2190 GBV_ILN_2232 GBV_ILN_2336 GBV_ILN_2446 GBV_ILN_2470 GBV_ILN_2472 GBV_ILN_2507 GBV_ILN_2522 GBV_ILN_2548 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4046 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4242 GBV_ILN_4246 GBV_ILN_4249 GBV_ILN_4251 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4313 GBV_ILN_4322 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4326 GBV_ILN_4328 GBV_ILN_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4336 GBV_ILN_4338 GBV_ILN_4393 GBV_ILN_4700 30.00 ASE 43.00 ASE AR 192 2020 12 12
language	English
source	Enthalten in Environmental monitoring and assessment 192(2020), 12 vom: Dez. volume:192 year:2020 number:12 month:12
sourceStr	Enthalten in Environmental monitoring and assessment 192(2020), 12 vom: Dez. volume:192 year:2020 number:12 month:12
format_phy_str_mv	Article
institution	findex.gbv.de
topic_facet	Turkey peloids Muds Peloidotherapy Mud therapy Clay
dewey-raw	333.7
isfreeaccess_bool	false
container_title	Environmental monitoring and assessment
authorswithroles_txt_mv	Özay, Pelin @@aut@@ Karagülle, Mine @@aut@@ Kardeş, Sinan @@aut@@ Karagülle, Müfit Zeki @@aut@@
publishDateDaySort_date	2020-12-01T00:00:00Z
hierarchy_top_id	31281738X
dewey-sort	3333.7
id	SPR042235502
language_de	englisch
fullrecord	<?xml version="1.0" encoding="UTF-8"?><collection xmlns="http://www.loc.gov/MARC21/slim"><record><leader>01000caa a22002652 4500</leader><controlfield tag="001">SPR042235502</controlfield><controlfield tag="003">DE-627</controlfield><controlfield tag="005">20220110232918.0</controlfield><controlfield tag="007">cr uuu---uuuuu</controlfield><controlfield tag="008">201203s2020 xx \|\|\|\|\|o 00\| \|\|eng c</controlfield><datafield tag="024" ind1="7" ind2=" "><subfield code="a">10.1007/s10661-020-08777-2</subfield><subfield code="2">doi</subfield></datafield><datafield tag="035" ind1=" " ind2=" "><subfield code="a">(DE-627)SPR042235502</subfield></datafield><datafield tag="035" ind1=" " ind2=" "><subfield code="a">(DE-599)SPRs10661-020-08777-2-e</subfield></datafield><datafield tag="035" ind1=" " ind2=" "><subfield code="a">(SPR)s10661-020-08777-2-e</subfield></datafield><datafield tag="040" ind1=" " ind2=" "><subfield code="a">DE-627</subfield><subfield code="b">ger</subfield><subfield code="c">DE-627</subfield><subfield code="e">rakwb</subfield></datafield><datafield tag="041" ind1=" " ind2=" "><subfield code="a">eng</subfield></datafield><datafield tag="082" ind1="0" ind2="4"><subfield code="a">333.7</subfield><subfield code="q">ASE</subfield></datafield><datafield tag="084" ind1=" " ind2=" "><subfield code="a">30.00</subfield><subfield code="2">bkl</subfield></datafield><datafield tag="084" ind1=" " ind2=" "><subfield code="a">43.00</subfield><subfield code="2">bkl</subfield></datafield><datafield tag="100" ind1="1" ind2=" "><subfield code="a">Özay, Pelin</subfield><subfield code="e">verfasserin</subfield><subfield code="4">aut</subfield></datafield><datafield tag="245" ind1="1" ind2="0"><subfield code="a">Chemical and mineralogical characteristics of peloids in Turkey</subfield></datafield><datafield tag="264" ind1=" " ind2="1"><subfield code="c">2020</subfield></datafield><datafield tag="336" ind1=" " ind2=" "><subfield code="a">Text</subfield><subfield code="b">txt</subfield><subfield code="2">rdacontent</subfield></datafield><datafield tag="337" ind1=" " ind2=" "><subfield code="a">Computermedien</subfield><subfield code="b">c</subfield><subfield code="2">rdamedia</subfield></datafield><datafield tag="338" ind1=" " ind2=" "><subfield code="a">Online-Ressource</subfield><subfield code="b">cr</subfield><subfield code="2">rdacarrier</subfield></datafield><datafield tag="520" ind1=" " ind2=" "><subfield code="a">Abstract To investigate the physical, chemical, and mineralogical characteristics of peloids, which are being used traditionally and historically across Turkey, and evaluate their suitability and potential for use in peloidotherapy. Five peloid samples were gathered from their places of origin, namely Gölemezli, Dalyan, Köprüköy, Gökçeada, and Dikili. Mineral analysis and physical and chemical analyses including electrical conductivity, density, cations, anions, trace elements, organic matters, and water retention capacity at 105 °C were performed. The peloids contained a combination of clay minerals (mainly montmorillonite, kaolinite, and muscovite) and non-clay minerals (mainly quartz, calcite, dolomite, and albite) except for Gölemezli peloid, which was dominated by calcite. The other minerals (i.e., chloride-serpentine, sphalerite, pyrite, magnesium calcite, cristobalite) were also found in some peloids. Gölemezli, Dalyan, and Köprüköy peloids had high total organic matters, mainly humic substances. The water retention capacity was high in Dalyan, Köprüköy, and Dikili peloids. All peloids had a pH value slightly greater than 7 (range 7.93–8.69). Dalyan, Köprüköy, and Dikili peloids had a high water retention capacity. Dalyan and Gökçeada peloids had a high electrical conductivity, 22.040 and 9.020 μS/cm, respectively. The density of peloids was ranged between 1.240 (Gölemezli) and 1.450 (Gökçeada) g/$ cm^{3} $. Total mineralization of investigated peloids was greater than 1000 mg/L: Köprüköy, 2754.8 mg/L; Gölemezli, 3092.8 mg/L; Dikili, 4044.6 mg/L; Gökçeada, 6576.6 mg/L; and Dalyan, 11782.9 mg/L, mainly sodium, magnesium, calcium, chloride, sulfate, bicarbonate, and metasilicic acid. The levels of trace elements were low (≤ 2.0 mg/L) in all peloids. The peloids contained various amounts of clay minerals (mainly montmorillonite, kaolinite, and muscovite), non-clay minerals (mainly quartz, calcite, dolomite, and albite), organic matters (mainly humic acid), cations (mainly sodium, magnesium, and calcium), anions (mainly chloride, sulfate, and bicarbonate), and insoluble compounds (mainly metasilicic acid). 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author	Özay, Pelin
spellingShingle	Özay, Pelin ddc 333.7 bkl 30.00 bkl 43.00 misc Turkey peloids misc Muds misc Peloidotherapy misc Mud therapy misc Clay Chemical and mineralogical characteristics of peloids in Turkey
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topic_title	333.7 ASE 30.00 bkl 43.00 bkl Chemical and mineralogical characteristics of peloids in Turkey Turkey peloids (dpeaa)DE-He213 Muds (dpeaa)DE-He213 Peloidotherapy (dpeaa)DE-He213 Mud therapy (dpeaa)DE-He213 Clay (dpeaa)DE-He213
topic	ddc 333.7 bkl 30.00 bkl 43.00 misc Turkey peloids misc Muds misc Peloidotherapy misc Mud therapy misc Clay
topic_unstemmed	ddc 333.7 bkl 30.00 bkl 43.00 misc Turkey peloids misc Muds misc Peloidotherapy misc Mud therapy misc Clay
topic_browse	ddc 333.7 bkl 30.00 bkl 43.00 misc Turkey peloids misc Muds misc Peloidotherapy misc Mud therapy misc Clay
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title	Chemical and mineralogical characteristics of peloids in Turkey
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title_full	Chemical and mineralogical characteristics of peloids in Turkey
author_sort	Özay, Pelin
journal	Environmental monitoring and assessment
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author_browse	Özay, Pelin Karagülle, Mine Kardeş, Sinan Karagülle, Müfit Zeki
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author-letter	Özay, Pelin
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title_sort	chemical and mineralogical characteristics of peloids in turkey
title_auth	Chemical and mineralogical characteristics of peloids in Turkey
abstract	Abstract To investigate the physical, chemical, and mineralogical characteristics of peloids, which are being used traditionally and historically across Turkey, and evaluate their suitability and potential for use in peloidotherapy. Five peloid samples were gathered from their places of origin, namely Gölemezli, Dalyan, Köprüköy, Gökçeada, and Dikili. Mineral analysis and physical and chemical analyses including electrical conductivity, density, cations, anions, trace elements, organic matters, and water retention capacity at 105 °C were performed. The peloids contained a combination of clay minerals (mainly montmorillonite, kaolinite, and muscovite) and non-clay minerals (mainly quartz, calcite, dolomite, and albite) except for Gölemezli peloid, which was dominated by calcite. The other minerals (i.e., chloride-serpentine, sphalerite, pyrite, magnesium calcite, cristobalite) were also found in some peloids. Gölemezli, Dalyan, and Köprüköy peloids had high total organic matters, mainly humic substances. The water retention capacity was high in Dalyan, Köprüköy, and Dikili peloids. All peloids had a pH value slightly greater than 7 (range 7.93–8.69). Dalyan, Köprüköy, and Dikili peloids had a high water retention capacity. Dalyan and Gökçeada peloids had a high electrical conductivity, 22.040 and 9.020 μS/cm, respectively. The density of peloids was ranged between 1.240 (Gölemezli) and 1.450 (Gökçeada) g/$ cm^{3} $. Total mineralization of investigated peloids was greater than 1000 mg/L: Köprüköy, 2754.8 mg/L; Gölemezli, 3092.8 mg/L; Dikili, 4044.6 mg/L; Gökçeada, 6576.6 mg/L; and Dalyan, 11782.9 mg/L, mainly sodium, magnesium, calcium, chloride, sulfate, bicarbonate, and metasilicic acid. The levels of trace elements were low (≤ 2.0 mg/L) in all peloids. The peloids contained various amounts of clay minerals (mainly montmorillonite, kaolinite, and muscovite), non-clay minerals (mainly quartz, calcite, dolomite, and albite), organic matters (mainly humic acid), cations (mainly sodium, magnesium, and calcium), anions (mainly chloride, sulfate, and bicarbonate), and insoluble compounds (mainly metasilicic acid). The physical, chemical, and mineralogical properties of peloids suggest their suitability and potential for use in peloidotherapeutic applications.
abstractGer	Abstract To investigate the physical, chemical, and mineralogical characteristics of peloids, which are being used traditionally and historically across Turkey, and evaluate their suitability and potential for use in peloidotherapy. Five peloid samples were gathered from their places of origin, namely Gölemezli, Dalyan, Köprüköy, Gökçeada, and Dikili. Mineral analysis and physical and chemical analyses including electrical conductivity, density, cations, anions, trace elements, organic matters, and water retention capacity at 105 °C were performed. The peloids contained a combination of clay minerals (mainly montmorillonite, kaolinite, and muscovite) and non-clay minerals (mainly quartz, calcite, dolomite, and albite) except for Gölemezli peloid, which was dominated by calcite. The other minerals (i.e., chloride-serpentine, sphalerite, pyrite, magnesium calcite, cristobalite) were also found in some peloids. Gölemezli, Dalyan, and Köprüköy peloids had high total organic matters, mainly humic substances. The water retention capacity was high in Dalyan, Köprüköy, and Dikili peloids. All peloids had a pH value slightly greater than 7 (range 7.93–8.69). Dalyan, Köprüköy, and Dikili peloids had a high water retention capacity. Dalyan and Gökçeada peloids had a high electrical conductivity, 22.040 and 9.020 μS/cm, respectively. The density of peloids was ranged between 1.240 (Gölemezli) and 1.450 (Gökçeada) g/$ cm^{3} $. Total mineralization of investigated peloids was greater than 1000 mg/L: Köprüköy, 2754.8 mg/L; Gölemezli, 3092.8 mg/L; Dikili, 4044.6 mg/L; Gökçeada, 6576.6 mg/L; and Dalyan, 11782.9 mg/L, mainly sodium, magnesium, calcium, chloride, sulfate, bicarbonate, and metasilicic acid. The levels of trace elements were low (≤ 2.0 mg/L) in all peloids. The peloids contained various amounts of clay minerals (mainly montmorillonite, kaolinite, and muscovite), non-clay minerals (mainly quartz, calcite, dolomite, and albite), organic matters (mainly humic acid), cations (mainly sodium, magnesium, and calcium), anions (mainly chloride, sulfate, and bicarbonate), and insoluble compounds (mainly metasilicic acid). The physical, chemical, and mineralogical properties of peloids suggest their suitability and potential for use in peloidotherapeutic applications.
abstract_unstemmed	Abstract To investigate the physical, chemical, and mineralogical characteristics of peloids, which are being used traditionally and historically across Turkey, and evaluate their suitability and potential for use in peloidotherapy. Five peloid samples were gathered from their places of origin, namely Gölemezli, Dalyan, Köprüköy, Gökçeada, and Dikili. Mineral analysis and physical and chemical analyses including electrical conductivity, density, cations, anions, trace elements, organic matters, and water retention capacity at 105 °C were performed. The peloids contained a combination of clay minerals (mainly montmorillonite, kaolinite, and muscovite) and non-clay minerals (mainly quartz, calcite, dolomite, and albite) except for Gölemezli peloid, which was dominated by calcite. The other minerals (i.e., chloride-serpentine, sphalerite, pyrite, magnesium calcite, cristobalite) were also found in some peloids. Gölemezli, Dalyan, and Köprüköy peloids had high total organic matters, mainly humic substances. The water retention capacity was high in Dalyan, Köprüköy, and Dikili peloids. All peloids had a pH value slightly greater than 7 (range 7.93–8.69). Dalyan, Köprüköy, and Dikili peloids had a high water retention capacity. Dalyan and Gökçeada peloids had a high electrical conductivity, 22.040 and 9.020 μS/cm, respectively. The density of peloids was ranged between 1.240 (Gölemezli) and 1.450 (Gökçeada) g/$ cm^{3} $. Total mineralization of investigated peloids was greater than 1000 mg/L: Köprüköy, 2754.8 mg/L; Gölemezli, 3092.8 mg/L; Dikili, 4044.6 mg/L; Gökçeada, 6576.6 mg/L; and Dalyan, 11782.9 mg/L, mainly sodium, magnesium, calcium, chloride, sulfate, bicarbonate, and metasilicic acid. The levels of trace elements were low (≤ 2.0 mg/L) in all peloids. The peloids contained various amounts of clay minerals (mainly montmorillonite, kaolinite, and muscovite), non-clay minerals (mainly quartz, calcite, dolomite, and albite), organic matters (mainly humic acid), cations (mainly sodium, magnesium, and calcium), anions (mainly chloride, sulfate, and bicarbonate), and insoluble compounds (mainly metasilicic acid). The physical, chemical, and mineralogical properties of peloids suggest their suitability and potential for use in peloidotherapeutic applications.
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container_issue	12
title_short	Chemical and mineralogical characteristics of peloids in Turkey
url	https://dx.doi.org/10.1007/s10661-020-08777-2
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author2	Karagülle, Mine Kardeş, Sinan Karagülle, Müfit Zeki
author2Str	Karagülle, Mine Kardeş, Sinan Karagülle, Müfit Zeki
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doi_str	10.1007/s10661-020-08777-2
up_date	2024-07-04T01:21:42.325Z
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Chemical and mineralogical characteristics of peloids in Turkey

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