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Artykuły w czasopismach na temat "Hydrochemistry"

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Zabokrytska, M. R. "“ESSAYS ON THE HISTORY OF HYDROCHEMISTRY IN UKRAINE” (2020) – THE FIRST MONOGRAPH ON THE HISTORY OF HYDROCHEMICAL STUDIES IN UKRAINE". Hydrology, hydrochemistry and hydroecology, nr 3 (58) (2020): 112–21. http://dx.doi.org/10.17721/2306-5680.2020.3.11.

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The article analyzes the monograph Essays on the History of Hydrochemistry in Ukraine (author Valentyn Khilchevskyi – professor at Taras Shevchenko National University of Kyiv), published in 2020.This is the first such monographic study. The monograph is devoted to the history of hydrochemical studies of surface waters in Ukraine. In the introductory part, an excursion on this issue was carried out in the XVIII-XIX centuries. The first part of the book is devoted to a review of hydrochemical studies of surface waters and their quality, which were carried out by Ukrainian scientists of the institutes of the National Academy of Sciences of Ukraine, industry institutions and institutions of higher education (1920-2020). As the author of the monograph notes, today scientific hydrochemical schools have been preserved at the Institute of Hydrobiology of the NAS of Ukraine (Kyiv), the Ukrainian Hydrometeorological Institute of the State Emergency Service of Ukraine and the NAS of Ukraine (Kyiv). They are engaged in hydrochemistry at the Ukrainian Institute of Environmental Problems (Kharkov). Among the higher educational institutions, it is worth noting the scientific hydrochemical school of the Taras Shevchenko National University of Kyiv, which has a prominent place in the development of the educational and methodological base, the creation of the first basic textbooks on hydrochemistry in Ukraine. They deal with individual issues of hydrochemistry at Odessa State Ecological University, Oles Honchar Dnipro National University, Yuriy Fedkovich Chernivtsi National University, Lesya Ukrainka Eastern European National University (Lutsk), National University of Water Management and Nature Management (Rivne). The second part describes the formation and history of the scientific hydrochemical school of the Taras Shevchenko National University of Kyiv (1970-2020), to which the author himself belongs. The information and facts presented in the monograph will be of extreme value from the standpoint of studying the history of hydrochemistry by young scientists, since today there is a reform in science and education, new concepts and terms are being introduced. For example, the nomenclature of the names of specialties is changing. So, the recruitment of graduate students of hydrologists-hydrochemists since 2016 is already carried out in specialty 103 “Earth Sciences” to the educational and scientific program “Hydrology”. And from 2021, it is planned to completely switch to a new form of defense of dissertations (in particular, the degree of candidate of sciences will be replaced by the degree of Doctor of Philosophy). The book will be useful to scientists and practitioners dealing with issues of hydrochemistry and water quality, teachers and students studying hydrochemical and hydroecological disciplines.
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Brown, Giles H. "Glacier meltwater hydrochemistry". Applied Geochemistry 17, nr 7 (lipiec 2002): 855–83. http://dx.doi.org/10.1016/s0883-2927(01)00123-8.

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Trudgill, Stephen. "Book Review: Hydrochemistry". Progress in Physical Geography: Earth and Environment 24, nr 1 (marzec 2000): 149–50. http://dx.doi.org/10.1177/030913330002400117.

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Church, M. Robbins. "HYDROCHEMISTRY OF FORESTED CATCHMENTS". Annual Review of Earth and Planetary Sciences 25, nr 1 (maj 1997): 23–59. http://dx.doi.org/10.1146/annurev.earth.25.1.23.

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Yanin, E. P., L. I. Kashina i Yu E. Sayet. "Hydrochemistry of Lake Glubokoe". Hydrobiologia 141, nr 1-2 (październik 1986): 11–23. http://dx.doi.org/10.1007/bf00007476.

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KHAFIZOV, A. R., L. A. КАМАLETDINOVA, A. F. KHAZIPOVA i A. V. КОМISSAROV. "Current state and long-term changes in the hydrochemistry of the Pavlovsky reservoir on the Ufa river". Prirodoobustrojstvo, nr 3 (2022): 101–7. http://dx.doi.org/10.26897/1997-6011-2022-3-101-107.

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The purpose of the work is to identify the current state and long-term changes in the hydrochemistry of the Pavlovsky reservoir, which allow further development of programs for its environmental rehabilitation. An analysis of studies of the current state and long-term changes in hydrochemistry (the content of chemical elements in water) of the Pavlovsky reservoir for 10 chemical indicators in 7 sites is presented. The factors that form and change the hydrochemistry of the Pavlovsky reservoir are studied. It was revealed that throughout the reservoir, from its beginning to the upper stream, the content of Sr2+, Mn2+ and petroleum products in the water decreases; increase – Zn2+, Hg2+, phenols and organic substances; are evenly distributed – Fettl (Fe2+ + Fe3+), Pttl (according to PO4 3-), Cu2+. A long-term trend of reducing the content of chemical elements in water is noted for Fe, Mn2+, petroleum products, phenols, COD; upward trend – for Rttl, Cu2+, Zn2+, phenols. The relationship between the average annual content of chemical elements in water and the values of average annual imflows has been established. Based on the results obtained, priority ways to improve the hydrochemistry of the Pavlovsky reservoir have been identified.
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Zhang, Hongying, Zongjun Gao, Mengjie Shi, Shaoyan Fang, Hailong Xu, Yechen Cui i Jiutan Liu. "Study of the Effects of Land Use on Hydrochemistry and Soil Microbial Diversity". Water 11, nr 3 (5.03.2019): 466. http://dx.doi.org/10.3390/w11030466.

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The objectives of this study were to compare the influence of land use, to determine which land has an impact on hydrochemistry and to clarify the impact of land use on soil microbial diversity and the correlation between hydrochemistry and soil microbial diversity. The impacts were assessed through chemical and biological data from 4 land-use groups. The results showed that soil microbial diversity and water chemical composition were different under different land uses. There was a strong correlation between the main hydrochemical components under different land uses, and the M03 had the highest correlation. The Shannon index was the largest for M01, the Simpson index was the smallest for M01, and the Chao1 and Ace indexes were the largest for M02. Actinobacteria, Proteobacteria and Acidobacteria were the dominant bacteria with different land uses, and some bacteria were present or absent depending on the land use. It was found that the soil CO2 content was different with different land uses. Soil CO2 content, hydrochemistry and soil microbial species were related to each other. A heatmap analysis showed that the F− and soil CO2 content showed a strong correlation with soil microorganisms and that the dominant bacteria were positively correlated. Under different land uses, hydrochemistry, soil CO2 and soil microorganisms interact with one another.
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Khilchevskyi, V. K. "GENERALIZED LIST OF PUBLICATIONS IN THE SCIENTIFIC COLLECTION “HYDROLOGY, HYDROCHEMISTRY AND HYDROECOLOGY” FOR 2016-2020". Hydrology, hydrochemistry and hydroecology, nr 2 (57) (2020): 88–104. http://dx.doi.org/10.17721/2306-5680.2020.2.2.

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The list of publications in the scientific periodical collection “Hydrology, hydrochemistry and hydroecology” for 2016-2020 is given. The scientific collection “Hydrology, hydrochemistry and hydroecology” was founded in May 2000 at the Taras Shevchenko National University of Kiev. In 2009, the collection was registered with the Ministry of Justice of Ukraine. The last recertification at the Ministry of Education and Science of Ukraine was in 2016 – the collection is included in the list of specialized scientific publications of Ukraine in the field of “Geographical Sciences”.In the formation of the collection of articles are grouped into five main sections: general methodological aspects of research; hydrology, water resources; hydrochemistry, hydroecology; hydroecology, hydrobiology; geographical aspects of hydroecological research. For the years 2016-2020. The collection contains about 270 publications. In total for the period 2000-2020. in 56 issues, about 1410 publications were published.
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Zabokrytska, M. R. "FIRST IN UKRAINE “HYDROCHEMICAL DICTIONARY” WAS PUBLISHED (2022)". Hydrology, hydrochemistry and hydroecology, nr 1(63) (2022): 71–74. http://dx.doi.org/10.17721/2306-5680.2022.1.7.

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The article presents and analyzes the scientific reference publication – “Hydrochemical Dictionary”, published by the professor of the Kiev National Taras Shevchenko University V.K. Khilchevskyi in 2022. Hydrochemistry is a scientific discipline that studies the chemical composition of natural waters (surface, underground and marine) and the patterns of its change depending on chemical, physical and biological processes occurring in the environment and under the influence of anthropogenic factors. Hydrochemistry has its own object of study, a theoretical, methodological and methodological basis, which allows it to develop important scientific and practical issues. It is closely connected with hydrology, geology, oceanology, and hydrobiology. Being formed in the process of formation and further development, hydrochemistry is constantly enriched with new terms and concepts. Yes, since the early 2000s. hydrochemical and hydroecological terminology has been influenced by the Water Framework Directive (WFD) of the European Union due to the deepening of international scientific contacts and the implementation in Ukraine of the provisions of the WFD in regulatory documents. Since an ever wider range of specialists is involved in this area, the issues of unification of hydrochemical terminology are becoming important. This goal is dedicated to the “Hydrochemical Dictionary”, which is the first in Ukraine scientific reference publication of this direction. The Dictionary includes terms widely used in the scientific literature on hydrochemistry, as well as a number of terms in related scientific disciplines related to hydrochemistry (hydrology, geography, hydrogeology, hydrobiology, analytical, organic and physical chemistry, geochemistry, etc.), the EU WFD. The “Hydrochemical Dictionary” contains terms covering the following issues: properties and chemical composition of natural waters; processes of formation of the chemical composition of natural waters; methodology and methods of hydrochemical research and water analysis; processes of pollution and self-purification of water bodies; hydrobiological and microbiological processes in water bodies; water quality and integrated water resources management. The Dictionary contains about 830 terms and concepts listed in the subject index, which makes it easy to find the right terms on the corresponding pages. “Hydrochemical Dictionary” is designed for students of universities specializing in “Earth Sciences” of educational programs of the hydrological profile, studying hydrochemical and hydroecological disciplines; will be useful to specialists in the field of hydrochemistry, hydrology, hydroecology, hydrogeology, geography.
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Shesterkin, V. P. "HYDROCHEMISTRY OF THE TYRMA RIVER". Regional problems 24, nr 2-3 (2021): 47–51. http://dx.doi.org/10.31433/2618-9593-2021-24-2-3-47-51.

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The spatial-temporal dynamics of the dissolved substances content in the Tyrma River water and in its tributaries have been studied by the author. It was found great differences in the values of mineralization and concentrations of HCO3-, Ca2+, Mg2+ and Fe, due to natural conditions of the territory.
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Rozprawy doktorskie na temat "Hydrochemistry"

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Butler, Catriona Elizabeth Hamilton. "Hydrochemistry of the Greenland Ice Sheet". Thesis, University of Bristol, 2014. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.683692.

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The subglacial environment of the Greenland Ice Sheet (GrIS) is poorly understood, in terms of hydrology, water storage and biogeochemical processes. High temporal resolution biogeochemical sampling of bulk meltwaters at a typical, land-terminating outlet glacier of the GrIS was employed in order to infer processes at the ice sheet bed over three contrasting melt seasons. No high temporal resolution geochemical datasets previously existed for ice sheet environments, mainly due to inaccessibility. Bulk meltwaters comprised differing propOltions of waters originating from a widespread, distributed subglacial drainage system (these delayed flow waters being solute enriched due to prolonged residence times and high rock:water ratios in the contributing environments), and an efficient channelized system (dilute surface waters rapidly transmitted to the margin). Two-component chemical mixing models, in combination with MODIS satellite imagery, revealed that delayed flow was released continuously. However, higher volumes were released at times of subglacial outburst events when draining surface lakes interacted with the bed and expelled stored waters. Dissolution experiments and geochemical data indicated that these waters may have been stored at the bed over winter, or longer, and comprised one-third of delayed flow release in any given year (~O.02 km\ The geochemical data, in combination with 01 80 -H20 isotope data from bulk meltwaters and surface ice, were able to identify subglacial drainage system evolution and increasingly distant water sources contributing to bulk meltwaters. Enhanced silicate dissolution was observed compared to smaller valley glaciers, which may lead to enhanced CO2 sequestration compared to carbonate weathering' environments. Chemical weathering rates were lower than would be expected for a poly thermal ice mass, likely due to low reactivity bedrock. Ionic fluxes were higher in high melt years, which is a further indication of stored water release due to extensive basal flushing. Finally, isotopes of sulphate demonstrated that there are both oxic and anoxic conditions at the bed of the GrIS, with potential for highly anoxic sulphate reducing conditions in the interior.
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Royston-Bishop, George William. "The hydrochemistry of subglacial Lake Vostok, Antarctica". Thesis, University of Bristol, 2006. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.431643.

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Jose, Paul V. "The hydrochemistry of backwaters and dead zones". Thesis, Loughborough University, 1988. https://dspace.lboro.ac.uk/2134/33160.

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This thesis investigates the inter-relationship between hydrological and water quality variations with reference to backwaters and dead zones in rivers. The examination of a series of controlled reservoir releases to an upland channel in Wales showed "in-channel" dead zones were important solute source and storage areas. Physico-chemical data have been presented to show the influence of main channel flow and quality variations on the hydrochemistry of a range of seven backwaters within the Trent basin. The hydrological regime of the mainstream seasonally modified backwater quality. The degree of main-flow influence declined with decreasing hydrological connectivity of the backwater environments with the mainstream. Furthermore other hydrological, biological and biogeochemical factors influenced backwater physico-chemistry. A generalised typology of permanent floodplain water bodies in the R. Trent catchment based upon water chemistry was established. An applied study examined the effect of reservoir cleaning/emptying operations and flood events on backwater hydrochemistry on the French Upper River Rhone. The simultaneous occurrence of decreasing mainstream discharge with the passage of the sediment laden release wave reduced its impact on backwater environments. Anthropogenic influences on riverine systems as a result of intensification of agriculture and urbanisation (e.g. nitrate pollution and river regulation) have influenced the hydrological and physico-chemical functioning of fluvial hydrosystems. In view of rising nitrate levels in many British rivers, trends within the Trent basin have been investigated. Rates of increase in concentration of 0.06 mg.l-1 N yr-1 were typical of rural catchments, whilst rates of up to 0.20 mg.l-1 N yr-1 were recorded in urbanised tributaries. Furthermore the impact of rising nitrate levels in the Trent catchment and river regulation on backwater hydrochemistry and ecology have been examined.
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Germer, Sonja. "Near-surface hydrology and hydrochemistry under contrasting land-cover". Phd thesis, Universität Potsdam, 2008. http://opus.kobv.de/ubp/volltexte/2008/1904/.

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Human transformation of the Earth’s land surface has far-reaching and important consequences for the functioning of hydrological and hydrochemical processes in watersheds. In nowadays land-use change from forest to pasture is a major issue in particular in the tropics. A sustainable management of deforested areas requires an in-depth understanding of the water and nutrient cycle. On this basis we compared the involved hydrological pathways for rainfall to reach streams and the nutrient budgets of a tropical rainforest and a pasture. In addition we studied the links of hydrochemical differences to differences of the relative importance of flowpaths. This study was conducted in the southwestern part of the Brazilian Amazon basin. An intensive hydrological and hydrochemical sampling and monitoring network was set up. The results indicate that the hydrology was modified in many ways due to land-use change. The most important alteration was the increased importance of the fast flowpath overland flow. Solute exports were in particular linked to the increased volume of overland flow that resulted from the land-use change. An additional reason for the increased nutrient exports from the pasture are the high concentrations of these nutrients in pasture overland flow probably as a due to cattle excrements. Tight nutrient cycles with minimal nutrient losses could not be maintained after the land-use change. This study provides the first attempt to quantify the respective nutrient losses.
Die Zerstörung von natürlicher Vegetation kann weit reichende Folgen auf den Wasser- und Nährstoffhaushalt von Ökosystemen haben. Der Landnutzungswandel vom Wald zur Weide ist heute in den Tropen ein wichtiges Thema. Eine nachhaltige Nutzung abgeholzter Gebiete setzt ein fundiertes Wissen des Wasser- und Nährstoffhaushaltes voraus. Darauf aufbauend wurden in dieser Studie das Abflussverhalten und die Nährstoffbilanzen von einem tropischem Regenwald und einer Weide verglichen. Außerdem wurde untersucht inwieweit die Nährstoffbilanzen vom Abflussverhalten abhängen. Die Untersuchungsgebiete liegen im südwestlichen brasilianischen Amazonasgebiet. Ein umfangreiches System zur Aufnahme von hydrologischen Daten und zum Sammeln von Wasserproben wurde aufgebaut. Die Ergebnisse haben gezeigt, dass sich das Abflussverhalten durch die Landnutzung geändert hat. Die wichtigste Änderung vom Wald zur Weide war der gesteigerte Anteil des schnellen Wasserabflusses auf der Geländeoberfläche. Hieraus resultierten gesteigerte Nährstoffausträge aus der Weide gegenüber dem Wald. Ein weiterer Grund für die gesteigerten Nährstoffausträge sind die hohen Konzentrationen dieser Stoffe im Oberflächenabfluss der Weide, die vermutlich mit den Ausscheidungen des Viehs zusammenhängen. Es hat sich also gezeigt, dass der quasi-geschlossene Nährstoffkreislauf nach der Landnutzungsänderung nicht aufrecht erhalten werden konnte. Diese Arbeit liefert den ersten Versuch diese Nährstoffverluste zur quantifizieren.
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Karim, Ajaz. "Hydrochemistry and isotope systematics of the Indus River Basin". Thesis, National Library of Canada = Bibliothèque nationale du Canada, 1999. http://www.collectionscanada.ca/obj/s4/f2/dsk1/tape8/PQDD_0010/NQ38787.pdf.

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Hutchins, Michael George. "Upland catchment hydrochemistry : an integrated modelling and field characterisation". Thesis, Imperial College London, 1996. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.338847.

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Harris, William Noel Laurence. "Controls on the likely hydrochemistry of subglacial Lake Ellsworth". Thesis, University of Bristol, 2014. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.665174.

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Since their discovery, subglacial lakes beneath the Antarctic ice sheet have been a focus of scientific curiosity and study. It has been postulated that subglacial lakes present a viable habitat for microbial life and are underlain by sediments containing a record of changes in the ice sheet above. Subglacial Lake Ellsworth, West Antarctica, is the subject of a continued project aiming to achieve clean access in order to explore these hypotheses. One of the key outcomes of lake sampling is to establish the hydrochemistry, from which deductions about the limnology of the system can be made. A new theoretical insight into the hydrochemistry of subglacial lakes is achieved through reanalysis of the geochemical dataset published from meteoric and accretion ice from above Subglacial Lake Vostok, East Antarctica. It is shown that Subglacial Lake Vostok is a well-mixed system at steady-state. Of the flux of water to the lake, ~60% drains away from the lake and ~40% freezes at the ice-water interface. A downstream subglacial hydrological catchment is strongly indicated. An average cationic denudation rate of ~9meq∑+·m-2·yr-1 is inferred at the lake-sediment interface. The methods and outcomes of the Subglacial Lake Vostok model form the theoretical basis to scope the controls on the hydrochemistry of Subglacial Lake Ellsworth. A hydrologically open lake system leads to dilute, isotopically heavier water. A hydrologically more isolated lake system results in more concentrated waters with a stable water isotope composition that is removed from the local meteoric water line. Geochemical weathering reactions are expected to contribute the majority of dissolved ionic species and meteoric ice is shown to deliver oxygen and nitrogen to the lake. The model results provide a theoretical framework for the interpretation of analyses from lake water samples. The model results are also used to guide a sampling and analysis strategy which would optimise the scientific gains of subglacial lake sampling. The precise nature of the processes within Subglacial Lakes Ellsworth and Vostok remain untested, but this thesis provides a robust basis for interpreting the hydrochemistry of both lakes.
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Lamb, Helen Rachel. "Chemical weathering in Alpine subglacial environments". Thesis, University of Bristol, 1997. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.387999.

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Tresch, Eliane. "Hydrochemistry of the Damma glacier forefield temporal and spatial variability /". Zurich : ETH Zurich, Department of Environmental Sciences, Institute of Biogeochemistry and Pollutant Dynamics, 2007. http://e-collection.ethbib.ethz.ch/show?type=dipl&nr=356.

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Elsenbeer, Helmut, Adam West i Mike Bonell. "Hydrologic pathways and stormflow hydrochemistry at South Creek, northeast Queensland". Universität Potsdam, 1994. http://opus.kobv.de/ubp/volltexte/2008/1690/.

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Earlier investigations at South Creek in northeastern Queensland established the importance of overland flow as a hydrologic pathway in this tropical rainforest environment. Since this pathway is ‘fast’, transmitting presumably ‘new’ water, its importance should be reflected in the stormflow chemistry of South Creek: the greater the volumentric contribution to the stormflow hydrograph, the more similarity between the chemical composition of streamwater and of overland flow is to be expected. Water samples were taken during two storm events in an ephemeral gully (gully A), an intermittent gully (gully B) and at the South Creek catchment outlet; additional spot checks were made in several poorly defined rills. The chemical composition of ‘old’ water was determined from 45 baseflow samples collected throughout February. The two events differed considerably in their magnitudes, intensities and antecedent moisture conditions. In both events, the stormflow chemistry in South Creek was characterized by a sharp decrease in Ca, Mg, Na, Si, Cl, EC, ANC, alkalinity and total inorganic carbon. pH remained nearly constant with discharge, whereas K increased sharply, as did sulfate in an ill-defined manner. In event 1, this South Creek stormflow pattern was closely matched by the pattern in gully A, implying a dominant contribution of ‘new’ water. This match was confirmed by the spot samples from rills. Gully B behaved like South Creek itself, but with a dampened ‘new’ water signal, indicating less overland flow generation in its subcatchment. In event 2, which occurred five days later, the initial ‘new’ water signal in gully A was rapidly overwhelmed by a different signal which is attributed to rapid drainage from a perched water table. This study shows that stormflow in this rainforest catchment consists predominantly of ‘new’ water which reaches the stream channel via ‘fast’ pathways. Where the ephemeral gullies delivering overland flow are incised deeply enough to intersect a perched water table, a delayed, ‘old’ water-like signal may be transmitted.
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Książki na temat "Hydrochemistry"

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M, Sharp, Richards K. S i Tranter M, red. Glacier hydrology and hydrochemistry. Chichester: J.Wiley, 1998.

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Eriksson, Erik. Principles and Applications of Hydrochemistry. Dordrecht: Springer Netherlands, 1985. http://dx.doi.org/10.1007/978-94-009-4836-5.

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Principles and applications of hydrochemistry. London: Chapman and Hall, 1985.

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W, Lloyd J. Aspects of hydrogeology and hydrochemistry. Birmingham: University of Birmingham, 1985.

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Nõges, Tiina. Lake Peipsi: Meteorology, hydrology, hydrochemistry. Tartu: Sulemees, 2001.

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Hasnain, Syed Iqbal. Himalayan glaciers: Hydrology and hydrochemistry. New Delhi: Allied Publishers, 1999.

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Marcy, A. D. Hydrochemistry of an inactive uranium mine. S.l: s.n, 1993.

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Jocelyne, Hughes, i Heathwaite A. L, red. Hydrology and hydrochemistry of British wetlands. Chichester: Wiley, 1995.

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A, Heathcote J., red. Natural inorganic hydrochemistry in relation to groundwater: An introduction. Oxford [Oxfordshire]: Clarendon Press, 1985.

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Berndt, Marian P. Hydrochemistry of the surficial and intermediate aquifer systems in Florida. Tallahassee, Fla: U.S. Dept. of the Interior, U.S. Geological Survey, 1993.

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Części książek na temat "Hydrochemistry"

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Por, F. D. "Hydrochemistry". W The Pantanal of Mato Grosso (Brazil), 31–33. Dordrecht: Springer Netherlands, 1995. http://dx.doi.org/10.1007/978-94-011-0031-1_11.

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Şen, Zekâi. "Hydrochemistry". W Earth Systems Data Processing and Visualization Using MATLAB, 115–41. Cham: Springer International Publishing, 2019. http://dx.doi.org/10.1007/978-3-030-01542-8_5.

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Eriksson, Erik. "Principles of hydrochemistry". W Principles and Applications of Hydrochemistry, 3–30. Dordrecht: Springer Netherlands, 1985. http://dx.doi.org/10.1007/978-94-009-4836-5_2.

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Yanin, E. P., L. I. Kashina i Yu E. Sayet. "Hydrochemistry of Lake Glubokoe". W Lake Glubokoe, 11–23. Dordrecht: Springer Netherlands, 1987. http://dx.doi.org/10.1007/978-94-009-4041-3_3.

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Pachajanov, D. N., D. L. Patina i N. I. Volkova. "Hydrochemistry of Lakes of Tajikistan". W Lake Issyk-Kul: Its Natural Environment, 169–79. Dordrecht: Springer Netherlands, 2002. http://dx.doi.org/10.1007/978-94-010-0491-6_13.

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Eriksson, Erik. "Environmental isotopes in hydrology and hydrochemistry". W Principles and Applications of Hydrochemistry, 103–15. Dordrecht: Springer Netherlands, 1985. http://dx.doi.org/10.1007/978-94-009-4836-5_5.

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Eriksson, Erik. "Applications of hydrochemistry and environmental isotopes". W Principles and Applications of Hydrochemistry, 116–75. Dordrecht: Springer Netherlands, 1985. http://dx.doi.org/10.1007/978-94-009-4836-5_6.

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Dassargues, Alain. "Introduction to groundwater quality and hydrochemistry". W Hydrogeology, 173–201. First Edition. | Boca Raton, Florida : Taylor & Francis, A CRC title, part of the Taylor & Francis imprint, a member of the Taylor & Francis Group, the academic division of T&F Informa plc, [2019]: CRC Press, 2018. http://dx.doi.org/10.1201/9780429470660-7.

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Maliva, Robert G. "MAR Hydrogeological and Hydrochemistry Evaluation Techniques". W Springer Hydrogeology, 243–85. Cham: Springer International Publishing, 2019. http://dx.doi.org/10.1007/978-3-030-11084-0_9.

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Eriksson, Erik. "Introduction". W Principles and Applications of Hydrochemistry, 1–2. Dordrecht: Springer Netherlands, 1985. http://dx.doi.org/10.1007/978-94-009-4836-5_1.

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Streszczenia konferencji na temat "Hydrochemistry"

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Kamilova, E., i G. Rakhmatkariev. "Medico-ecological aspects of hydrochemistry of Uzbekistan". W Environmental Health Risk 2001. Southampton, UK: WIT Press, 2001. http://dx.doi.org/10.2495/ehr010121.

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Shesterkin, V. P., i I. V. Kostomarova. "GROUNDWATER HYDROCHEMISTRY OF THE BOTCHI RIVER BASIN". W The Geological Evolution of the Water-Rock Interaction. Buryat Scientific Center of SB RAS Press, 2018. http://dx.doi.org/10.31554/978-5-7925-0536-0-2018-207-209.

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Shesterkin, V. P. "HYDROCHEMISTRY OF KARST WATERS OF TUKURINGA-JAGDINSKY MASSIF". W The Geological Evolution of the Water-Rock Interaction. Buryat Scientific Center of SB RAS Press, 2018. http://dx.doi.org/10.31554/978-5-7925-0536-0-2018-205-206.

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Zawawi, Mohd Hafiz, Mohamad Anuar Kamaruddin, Mohd Zakwan Ramli i Md Shabbir Hossain. "Shallow groundwater hydrochemistry assessment of engineered landfill and dumpsite". W THE 3RD ISM INTERNATIONAL STATISTICAL CONFERENCE 2016 (ISM-III): Bringing Professionalism and Prestige in Statistics. Author(s), 2017. http://dx.doi.org/10.1063/1.4983794.

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Yang, Qiu, Honglang Xiao, Zhengliang Yin i Heng Wei. "Hydrochemistry Characteristics of Groundwater in Agricultural Oasis Areas, Northwest China". W Environment and Water Resource Management. Calgary,AB,Canada: ACTAPRESS, 2014. http://dx.doi.org/10.2316/p.2014.812-011.

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Bonotto, D. M., i E. G. Oliveira. "Flow rate and hydrochemistry in areas of sand mining activities". W WATER POLLUTION 2006. Southampton, UK: WIT Press, 2006. http://dx.doi.org/10.2495/wp060111.

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Townsend, Kambray, Laura J. Crossey, Karl Karlstrom, Brittany Griego i Livia Crowley. "Hydrochemistry of an Alpine Karst System, Northern New Mexico: Las Huertas". W 2023 New Mexico Geological Society Annual Spring Meeting. Socorro, NM: New Mexico Geological Society, 2023. http://dx.doi.org/10.56577/sm-2023.2944.

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Townsend, Kambray, Laura Crossey, Karl Karlstrom, Brittany Griego i Livia Crowley. "HYDROCHEMISTRY OF AN ALPINE KARST SYSTEM, NORTHERN NEW MEXICO: LAS HUERTAS". W GSA Connects 2022 meeting in Denver, Colorado. Geological Society of America, 2022. http://dx.doi.org/10.1130/abs/2022am-378537.

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Drummond, Margaret G., Arianna C. Camarena, Arianna C. Camarena, Barry Hibbs, Barry Hibbs, Lillian E. Alwood, Lillian E. Alwood, Johnathan Alexander i Johnathan Alexander. "ISOTOPE HYDROLOGY AND HYDROCHEMISTRY OF THE UPPER LOS ANGELES RIVER, CA". W GSA Connects 2022 meeting in Denver, Colorado. Geological Society of America, 2022. http://dx.doi.org/10.1130/abs/2022am-382527.

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Wang, Maolan, Wenbin Zhou i Yongping Ai. "Notice of Retraction: The Hydrochemistry and Nutrient Distribution in Poyang Lake, China". W 2011 5th International Conference on Bioinformatics and Biomedical Engineering. IEEE, 2011. http://dx.doi.org/10.1109/icbbe.2011.5780914.

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Raporty organizacyjne na temat "Hydrochemistry"

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Grasby, S. Hydrochemistry of the Englishman River. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 2016. http://dx.doi.org/10.4095/298893.

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G. Patterson i P. Striffler. Vertical Variability in Saturated Zone Hydrochemistry Near Yucca Mountain, Nevada. Office of Scientific and Technical Information (OSTI), luty 2007. http://dx.doi.org/10.2172/899951.

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Trihey, J. M., E. S. B. McGrath-Cohen i A. M. Haiblen. Exploring for the Future—Hydrochemistry Data Release, Daly River project, Northern Territory. Geoscience Australia, 2020. http://dx.doi.org/10.11636/record.2020.046.

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Spane, F. A. Jr, i W. D. Webber. Hydrochemistry and hydrogeologic conditions within the Hanford Site upper basalt confined aquifer system. Office of Scientific and Technical Information (OSTI), wrzesień 1995. http://dx.doi.org/10.2172/111944.

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McGarth-Cohen, E. S. B., J. M. Trihey i J. Northey. Exploring for the Future—Groundwater hydrochemistry data release, Ti Tree project, Northern Territory. Geoscience Australia, 2020. http://dx.doi.org/10.11636/record.2020.044.

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McGarth-Cohen, E. S. B., J. M. Trihey i A. M. Haiblen. Exploring for the Future—Groundwater hydrochemistry data release, Howard East project, Northern Territory. Geoscience Australia, 2020. http://dx.doi.org/10.11636/record.2020.047.

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Trihey, J. M., i J. E. Northey. Exploring for the Future—Groundwater hydrochemistry data release: Western Davenport project, Northern Territory. Geoscience Australia, 2020. http://dx.doi.org/10.11636/record.2020.048.

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McGarth-Cohen, E. S. B., J. M. Trihey i J. E. Northey. Exploring for the Future—Groundwater hydrochemistry data release: Alice Springs project, Northern Territory. Geoscience Australia, 2020. http://dx.doi.org/10.11636/record.2020.045.

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Trihey, J. M., i C. Harris-Pascal. Exploring for the Future—Groundwater hydrochemistry data release: East Kimberley project, Northern Territory. Geoscience Australia, 2020. http://dx.doi.org/10.11636/record.2020.043.

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Brunton, F. R., E. H. Priebe i K. Yeung. Relating sequence stratigraphic and karstic controls of regional groundwater flow zones and hydrochemistry within the Early Silurian Lockport Group of the Niagara Escarpment, southern Ontario. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 2016. http://dx.doi.org/10.4095/297726.

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