Prošće湖泊集水区的土壤和沉积物作为湖泊系统中可能的陆源输入

IF 1 4区 地球科学 Q4 GEOSCIENCES, MULTIDISCIPLINARY Acta Carsologica Pub Date : 2020-01-01 DOI:10.3986/ac.v49i1.7547
A. P. Siročić, S. Kurajica, Dragana Dogančić, N. Fišter
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Samples of soil, peat and stream sediment were collected in the Prošće lake catchment and partly in the assumed zone of influence, X-ray diffraction (XRD) and Fourier Transform Infrared spectroscopy (FTIR) analysis of samples was performed to determine dominant mineral species in samples. XRD analysis showed predominance of lowquartz, which was found in all samples, most often as dominant phase. Dolomite was found in half of the samples, almost always as a significant phase while calcite was dominant phase in one of the samples. In most of the samples, members of the feldspars and chlorites groups, as well as muscovite, were present as minor phases. The absorption bands in the range of 2800-3000 cm-1 due to the organic matter are visible in spectra of all samples. These minerals can enter lakes system by surface waters, primarily streams and overland flow during snow thawing and rain, and also in cases of shore erosion. Terrigenic input in lakes is small but cannot be neglected due to the longlasting preservation efforts of the Prošće Lake recharge area, and the Plitvice Lakes National Park in general, terrigenous intake still does not pose a threat to water quality and tufa production. Izvleček UDKs 631.41:502.51(497.5Proščansko jezero) Anita Ptiček Siročić, Stanislav Kurajica, Dragana Dogančić & Nikolina Fišter: Tla in sedimenti zaledja Proščanskega jezera kot možen terigen doprinos v jezerski sistem Narodni park Plitviška jezera se nahaja v severozahodnem delu Dinarskega krasa v osrednji Hrvaški. Pomembna vloga tal v krasu je, da čistijo vodo, preden doseže freatično cono. Tla so tudi območje, kjer se potencialna onesnaževala kopičijo, preoblikujejo in redčijo. Tla ta onesnaževala tudi zadržijo. Poznavanje mineraloške sestave tal je pomemben dejavnik pri razumevanju prenosa onesnaževal v jezerskem sistemu. Tla, šoto in sedimente smo vzorčili v neposrednem zaledju in na vplivnem območju Prošćankega jezera. Mineralne vrste smo določili z rentgensko difrakcijo (XRD) in infrardečo spektroskopijo s Fourierjevo transformacijo (FTIR). Analiza XRD je pokazala, da v vzorcih prevladuje kremen, ki je bil v vseh vzorcih ugotovljen kot prevladujoč mineral. Dolomit je bil najden v polovici vzorcev, skoraj vedno kot pomemben mineral, medtem ko je kalcit prevladoval samo v enem od vzorcev. V večini vzorcev so bili v manjšini še glinenci, kloritni minerali in muskovit. Absorpcijski pasovi na območju 2800-3000 cm-1 so bili zaradi organske snovi vidni v vseh spektrih. Minerale lahko v jezerski sistem prinesejo površinske vode, predvsem med taljenjem snega in ob padavinah ali obalni herozijskih procesi. Terigeni vnos je majhen, vendar ga zaradi dolgotrajnih prizadevanj za ohranitev in obnovo območja Prošćanskega jezera ni mogoče prezreti. Verjetno pa še ne ogroža kakovosti vode in nastajanja lehnjaka. Rezultati kažejo, da tla in sedimenti v zaledju Proščanskega jezera učinkovito zadržijo in čistijo vodo na poti do jezera. Vseeno lahko ob morebitnem onesnaženju v zaledju onesnaževala dosežejo jezerski sistem, če so adsorbirana na delce tal. 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Samples of soil, peat and stream sediment were collected in the Prošće lake catchment and partly in the assumed zone of influence, X-ray diffraction (XRD) and Fourier Transform Infrared spectroscopy (FTIR) analysis of samples was performed to determine dominant mineral species in samples. XRD analysis showed predominance of lowquartz, which was found in all samples, most often as dominant phase. Dolomite was found in half of the samples, almost always as a significant phase while calcite was dominant phase in one of the samples. In most of the samples, members of the feldspars and chlorites groups, as well as muscovite, were present as minor phases. The absorption bands in the range of 2800-3000 cm-1 due to the organic matter are visible in spectra of all samples. These minerals can enter lakes system by surface waters, primarily streams and overland flow during snow thawing and rain, and also in cases of shore erosion. 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引用次数: 2

摘要

UDC 631.41:502.51(497.5Proščansko jezero) Anita ptiek siro iki, Stanislav Kurajica, Dragana dogan iki & Nikolina Fišter: Prošće湖泊集水区的土壤和沉积物可能是湖泊系统的陆源输入。Plitvice湖泊国家公园位于克罗地亚中部Dinaric喀斯特的西北部。喀斯特土壤的一个重要作用是在水到达潜水带之前对其进行净化。土壤也是潜在污染物积聚、转化、阻滞和稀释的区域。了解土壤矿物学成分是了解湖泊系统中污染物的命运和运移的重要因素。在Prošće湖泊集水区和部分假设影响区内采集土壤、泥炭和水系沉积物样品,对样品进行x射线衍射(XRD)和傅里叶变换红外光谱(FTIR)分析,确定样品中的优势矿物种类。XRD分析表明,所有样品均以低石英为主,且多为优势相。在一半的样品中发现白云石,几乎总是作为重要相,而方解石在一个样品中占主导地位。在大多数样品中,长石和绿泥石群的成员,以及白云母,作为小相存在。在所有样品的光谱中均可见到2800 ~ 3000 cm-1范围内有机质的吸收带。这些矿物质可以通过地表水进入湖泊系统,主要是在雪融化和雨融化期间的溪流和陆地流动,也可以在海岸侵蚀的情况下进入湖泊系统。由于Prošće湖泊补给区的长期保护工作,湖泊中的陆源输入很小,但不能忽视,总的来说,Plitvice湖泊国家公园的陆源输入仍然不会对水质和凝灰岩生产构成威胁。izvle ekudks 631.41:502.51(497.5Proščansko jezero) Anita ptiek siro伊奇,Stanislav Kurajica, Dragana dogan伊奇和Nikolina Fišter: Tla in sedimenti zaledja Proščanskega jezera kot možen terigen doprinos v jezerski系统Narodni公园Plitviška jezera se nahaja v severozahodnem delu Dinarskega krasa v osrednji Hrvaški。Pomembna vloga tal v krasu je, da istijo vodo, preden doseže freatiati no cono。Tla so tudi obmo je, kjer se potenticialna onesnaževala kopi ijo, preoblikujejo in red ijo。Tla ta onesnaževala tudi zadržijo。波兹纳瓦涅mineraloške sestave tal je pomemben dejavnik pri razumevanju prenosa onesnaževal v jezerskem sistemu。1 . šoto in sediment smo vzor v neposrednem zaledju in na vplivnem obmo ju Prošćankega jezera。矿物学研究表明,矿物学研究的主要内容是利用红外光谱法(FTIR)分析矿物学研究的成果。分析XRD je pokazala, da v vzorcih prevladuje kremen, ki je bil v vzorcih vzorcih ugotovljen kot prevladujoza矿物。dolomet je biljden v polovici vzorcev, skoraj vedno kot pommenbeni mineral, medtem ko je kalciv preladv v neem od vzorcev。V veini vzorcev so bili V manjšini še glinenci, kloritni minerali在muskovit。吸收pcijski pasovi na obmo为2800-3000 cm-1,因此,可以用光谱法测定生物器官的积雪。Minerale lahko v jezerski系统prinesejo površinske vode, predvsem taljenjem snega in ob padavinah ali obalni herozijskih process。Terigeni vnos je majhen, vendar ga zaradi dolgotrajnih prizaddevanj za ohranitev in obnovo obmo ja Prošćanskega jezera ni mogo e prezreti。Verjetno pa še ne ogroža kakovosti vode in nastajanja lehnjaka。Rezultati kažejo, da tla in sedimenti v zaledju Proščanskega jezera u inkovito zadržijo in istijo vodo na poti do jezera。Vseeno lahko ob morebitnem onesnaženju v zaledju onesnaževala dosežejo jezerski系统, e so吸附剂na delce tal。1萨格勒布大学岩土工程学院,哈勒罗瓦,阿列哈,472000 Varaždin, e-mail: aanitaps@gfv.unizg.hr;ddogan@gfv.unizg.hr;nfister@hotmail.com 2萨格勒布大学化学工程技术学院,Marulićev trg 19, 10000萨格勒布,e-mail: stankok@fkit.hr *通讯作者收稿/预稿日期:25.07.2019 DOI: 10.3986/ac.v49i1.7547 ACTA cars49 / 1,125 -140, POSTOJNA 2020 COBISS: 1.01 ANITA PTIČEK SIROČIĆ, STANISLAV KURAJICA, DRAGANA DOGANČIĆ & NIKOLINA FIŠTER
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Soils and sediments of Prošće Lake catchment as a possible terrigenous input in the lakes system
UDC 631.41:502.51(497.5Proščansko jezero) Anita Ptiček Siročić, Stanislav Kurajica, Dragana Dogančić & Nikolina Fišter: Soils and sediments of Prošće Lake catchment as a possible terrigenous input in the lakes system The Plitvice Lakes National Park is in the northwestern part of the Dinaric Karst in central Croatia. An important role of the soil in the karst is to purify the waters before they reach the phreatic zone. The soil is also a zone of accumulation, transformation, retardation and dilution of a potential pollutant. Knowing soil mineralogical composition is an important factor in understanding fate and transport of contaminants throughout lakes system. Samples of soil, peat and stream sediment were collected in the Prošće lake catchment and partly in the assumed zone of influence, X-ray diffraction (XRD) and Fourier Transform Infrared spectroscopy (FTIR) analysis of samples was performed to determine dominant mineral species in samples. XRD analysis showed predominance of lowquartz, which was found in all samples, most often as dominant phase. Dolomite was found in half of the samples, almost always as a significant phase while calcite was dominant phase in one of the samples. In most of the samples, members of the feldspars and chlorites groups, as well as muscovite, were present as minor phases. The absorption bands in the range of 2800-3000 cm-1 due to the organic matter are visible in spectra of all samples. These minerals can enter lakes system by surface waters, primarily streams and overland flow during snow thawing and rain, and also in cases of shore erosion. Terrigenic input in lakes is small but cannot be neglected due to the longlasting preservation efforts of the Prošće Lake recharge area, and the Plitvice Lakes National Park in general, terrigenous intake still does not pose a threat to water quality and tufa production. Izvleček UDKs 631.41:502.51(497.5Proščansko jezero) Anita Ptiček Siročić, Stanislav Kurajica, Dragana Dogančić & Nikolina Fišter: Tla in sedimenti zaledja Proščanskega jezera kot možen terigen doprinos v jezerski sistem Narodni park Plitviška jezera se nahaja v severozahodnem delu Dinarskega krasa v osrednji Hrvaški. Pomembna vloga tal v krasu je, da čistijo vodo, preden doseže freatično cono. Tla so tudi območje, kjer se potencialna onesnaževala kopičijo, preoblikujejo in redčijo. Tla ta onesnaževala tudi zadržijo. Poznavanje mineraloške sestave tal je pomemben dejavnik pri razumevanju prenosa onesnaževal v jezerskem sistemu. Tla, šoto in sedimente smo vzorčili v neposrednem zaledju in na vplivnem območju Prošćankega jezera. Mineralne vrste smo določili z rentgensko difrakcijo (XRD) in infrardečo spektroskopijo s Fourierjevo transformacijo (FTIR). Analiza XRD je pokazala, da v vzorcih prevladuje kremen, ki je bil v vseh vzorcih ugotovljen kot prevladujoč mineral. Dolomit je bil najden v polovici vzorcev, skoraj vedno kot pomemben mineral, medtem ko je kalcit prevladoval samo v enem od vzorcev. V večini vzorcev so bili v manjšini še glinenci, kloritni minerali in muskovit. Absorpcijski pasovi na območju 2800-3000 cm-1 so bili zaradi organske snovi vidni v vseh spektrih. Minerale lahko v jezerski sistem prinesejo površinske vode, predvsem med taljenjem snega in ob padavinah ali obalni herozijskih procesi. Terigeni vnos je majhen, vendar ga zaradi dolgotrajnih prizadevanj za ohranitev in obnovo območja Prošćanskega jezera ni mogoče prezreti. Verjetno pa še ne ogroža kakovosti vode in nastajanja lehnjaka. Rezultati kažejo, da tla in sedimenti v zaledju Proščanskega jezera učinkovito zadržijo in čistijo vodo na poti do jezera. Vseeno lahko ob morebitnem onesnaženju v zaledju onesnaževala dosežejo jezerski sistem, če so adsorbirana na delce tal. Pozna1 Faculty of Geotechnical Engineering, University of Zagreb, Hallerova aleja 7, 42000 Varaždin, e-mail: aanitaps@gfv.unizg.hr; ddogan@gfv.unizg.hr; nfister@hotmail.com 2 Faculty of Chemical Engineering and Technology, University of Zagreb, Marulićev trg 19, 10000 Zagreb, e-mail: stankok@fkit.hr * Corresponding Author Received/Prejeto: 25.07.2019 DOI: 10.3986/ac.v49i1.7547 ACTA CARSOLOGICA 49/1, 125-140, POSTOJNA 2020 COBISS: 1.01 ANITA PTIČEK SIROČIĆ, STANISLAV KURAJICA, DRAGANA DOGANČIĆ & NIKOLINA FIŠTER
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来源期刊
Acta Carsologica
Acta Carsologica 地学-地球科学综合
CiteScore
1.50
自引率
14.30%
发文量
0
审稿时长
>12 weeks
期刊介绍: Karst areas occupy 10-20 % of ice-free land. Dissolution of rock by natural waters has given rise to specific landscape and underground. Karst surface features and caves have attracted man''s curiosity since the dawn of humanity and have been a focus to scientific studies since more than half of millennia. Acta Carsologica publishes original research papers and reviews, letters, essays and reports covering topics related to specific of karst areas. These comprise, but are not limited to karst geology, hydrology, and geomorphology, speleology, hydrogeology, biospeleology and history of karst science.
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