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Books on the topic 'High-salinity'

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Author: Grafiati

Published: 4 June 2021

Last updated: 1 February 2022

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1

Abdelly, Chedly, Münir Öztürk, Muhammad Ashraf, and Claude Grignon, eds. Biosaline Agriculture and High Salinity Tolerance. Basel: Birkhäuser Basel, 2008. http://dx.doi.org/10.1007/978-3-7643-8554-5.

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2

Khan, M. Ajmal, and Darrell J. Weber, eds. Ecophysiology of High Salinity Tolerant Plants. Dordrecht: Springer Netherlands, 2006. http://dx.doi.org/10.1007/1-4020-4018-0.

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3

Carter, J. P. Materials of construction for high-salinity geothermal brines. Washington, D.C: U.S. Dept. of the Interior, Bureau of Mines, 1992.

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4

Lieth, Helmut, and Ahmed A. Al Masoom, eds. Towards the rational use of high salinity tolerant plants. Dordrecht: Springer Netherlands, 1993. http://dx.doi.org/10.1007/978-94-011-1858-3.

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5

Lieth, Helmut, and Ahmed A. Al Masoom, eds. Towards the rational use of high salinity tolerant plants. Dordrecht: Springer Netherlands, 1993. http://dx.doi.org/10.1007/978-94-011-1860-6.

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6

Reese, Ronald S. Hydrogeologic and hydraulic characterization of the surficial aquifer system, and origin of high salinity groundwater, Palm Beach County, Florida. Reston, Va: U.S. Dept. of the Interior, U.S. Geological Survey, 2009.

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7

Yobbi, D. K. Effects of river discharge and high-tide stage on salinity intrusion in the Weeki Wachee, Crystal, and Withlacoochee River estuaries, southwest Florida. Tallahassee, Fla: Dept. of the Interior, U.S. Geological Survey, 1990.

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8

ASWAS Conference (1st 1990 United Arab Emirates University). Towards the rational use of high salinity tolerant plants: Proceedings of the First ASWAS Conference, December 8-15, 1990 at the United Arab Emirates University, Al Ain, United Arab Emirates. Dordrecht: Kluwer Academic, 1993.

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9

Montgomery, Ellyn T. Use of the High Resolution Profiler (HRP) in the Salt Finger Tracer Release Experiment (SFTRE). Woods Hole, Mass: Woods Hole Oceanographic Institution, 2002.

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10

Khan, M. Ajmal, and Darrell J. Weber. Ecophysiology of High Salinity Tolerant Plants. Springer, 2008.

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11

Ecophysiology of High Salinity Tolerant Plants. Springer, 2008.

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12

C, Abdelly, ed. Biosaline agriculture and high salinity tolerance. Basel: Birkhäuser, 2008.

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13

Ajmal, Khan M., and Weber Darrell J. 1933-, eds. Ecophysiology of high salinity tolerant plants. Dordrecht: Springer, 2006.

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14

Ajmal, Khan M., and Weber Darrell J. 1933-, eds. Ecophysiology of high salinity tolerant plants. Dordrecht: Springer, 2006.

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15

Lieth, Helmut. Towards the rational use of high salinity tolerant plants : Vol 1: Deliberations About High Salinity Tolerant Plants And Ecosystems. Springer, 2012.

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16

(Editor), H. Lieth, and A.A. Al Masoom (Editor), eds. Towards the Rational Use of High Salinity Tolerant Plants: Volume 1: Deliberations about High Salinity Tolerant Plants and Ecosystems (Tasks for Vegetation Science). Springer, 2007.

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17

G, Norton Jerrold, and Southwest Fisheries Science Center (U.S.), eds. Continuous high resolution shore station temperature and salinity data from Granite Canyon, California. [La Jolla, Calif.]: U.S. Dept. of Commerce, National Oceanic and Atmospheric Administration, National Marine Fisheries Service, Southwest Fisheries Science Center, 1999.

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18

(Editor), M. Ajmal Khan, and Darrell J. Weber (Editor), eds. Ecophysiology of High Salinity Tolerant Plants (Tasks for Vegetation Science) (Tasks for Vegetation Science). Springer, 2005.

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19

Dasgupta, Susmita, Md Moqbul Hossain, Mainul Huq, and David Wheeler. Climate Change, Soil Salinity, and the Economics of High-Yield Rice Production in Coastal Bangladesh. The World Bank, 2014. http://dx.doi.org/10.1596/1813-9450-7140.

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20

Park, Andrew D. Preconditioning responses of salt-tolerant and salt-sensitive provenances of Acacia tortilis (Forsk.) Hayne to high salinity. 1995.

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21

Henry, Mark A., and Avinash B. Kumar. Cerebral Salt Wasting. Edited by Matthew D. McEvoy and Cory M. Furse. Oxford University Press, 2017. http://dx.doi.org/10.1093/med/9780190226459.003.0068.

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Abstract:

Human survival (on a biochemical level) depends on the body’s critical ability to regulate the osmolality and salinity of extracellular fluid. When functioning in a normal state, the osmoregulatory system stringently maintains the serum sodium in a narrow range. Alterations in the serum sodium and water balance have significant and sometimes life-threatening impact on patients—especially when they occur in conjunction with serious intracranial pathology. This chapter, including the case discussion, illustrates the conundrum of hyponatremia and high urine output states complicating neurological illness. A thorough understanding of the pathophysiology, assessment, and treatment of these conditions is essential for the timely delivery of care and optimal patient outcomes.

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22

Aldous, David E., and Ian H. Chivers. Sports Turf and Amenity Grasses. CSIRO Publishing, 2002. http://dx.doi.org/10.1071/9780643090019.

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Sports Turf and Amenity Grasses is a comprehensive reference for anyone involved with the selection and maintenance of grasses used in sports and amenity areas in all areas. It provides a means to identify these grasses through keys, descriptions and photographs, and also provides detailed information on sowing, oversowing, stolonising and mowing heights. The performance of each grass is assessed and detailed comments made on positive and negative aspects of its use. A grass’s tolerance to high temperature, frost, drought, shade, wet soil, salinity, low soil fertility, wear and close mowing is given in a table with each aspect rated. Further comments are made on how well it combines with particular grasses and on issues such as seedling vigour and sowing times.

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23

Kalinin, A. A., Ye E. Savchenko, and V. Yu Prokofiev. Mineralogy and genesis of the Oleninskoe gold deposit (Kola Peninsula). FRC KSC RAS, 2021. http://dx.doi.org/10.37614/978.5.91137.446.4.

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Data on geology of the Oleninskoe deposit, and results of mineralogical and geochemical investigations of ores and altered rocks are presented. Mineralization is connected with granite porphyry sills, an end member of gabbrodiorite-diorite-granodiorite complex of minor intrusions. The main alteration processes are diopsidization and biotitization, formation of quartz-muscovite-albite, quartz-aresenopyrite-tourmaline, and quartz metasomatic rocks. More than 50 ore minerals (sulfides, sulfosalts, tellurides, and native metals) were identified in the ore, including 20 minerals of silver and gold. Mineral associations in the ore and sequence of mineral formation are defined. Five generations of gold-silver alloys are identified, its composition covers spectrum from native silver to high-grade gold. Mineralized fluids in the deposit are of high salinity (sodium and calcium chlorides), and rich in As, Sb, Pb, Cu, Zn, and Ag. The Oleninskoe deposit is classified as an epithermal metamorphosed gold deposit.The book is of interest for specialists in economic geology, mineralogy and geochemistry of ore deposits.

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24

Vuorinen, Ilppo. Post-Glacial Baltic Sea Ecosystems. Oxford University Press, 2018. http://dx.doi.org/10.1093/acrefore/9780190228620.013.675.

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Post-glacial aquatic ecosystems in Eurasia and North America, such as the Baltic Sea, evolved in the freshwater, brackish, and marine environments that fringed the melting glaciers. Warming of the climate initiated sea level and land rise and subsequent changes in aquatic ecosystems. Seminal ideas on ancient developing ecosystems were based on findings in Swedish large lakes of species that had arrived there from adjacent glacial freshwater or marine environments and established populations which have survived up to the present day. An ecosystem of the first freshwater stage, the Baltic Ice Lake initially consisted of ice-associated biota. Subsequent aquatic environments, the Yoldia Sea, the Ancylus Lake, the Litorina Sea, and the Mya Sea, are all named after mollusc trace fossils. These often convey information on the geologic period in question and indicate some physical and chemical characteristics of their environment. The ecosystems of various Baltic Sea stages are regulated primarily by temperature and freshwater runoff (which affects directly and indirectly both salinity and nutrient concentrations). Key ecological environmental factors, such as temperature, salinity, and nutrient levels, not only change seasonally but are also subject to long-term changes (due to astronomical factors) and shorter disturbances, for example, a warm period that essentially formed the Yoldia Sea, and more recently the “Little Ice Age” (which terminated the Viking settlement in Iceland).There is no direct way to study the post-Holocene Baltic Sea stages, but findings in geological samples of ecological keystone species (which may form a physical environment for other species to dwell in and/or largely determine the function of an ecosystem) can indicate ancient large-scale ecosystem features and changes. Such changes have included, for example, development of an initially turbid glacial meltwater to clearer water with increasing primary production (enhanced also by warmer temperatures), eventually leading to self-shading and other consequences of anthropogenic eutrophication (nutrient-rich conditions). Furthermore, the development in the last century from oligotrophic (nutrient-poor) to eutrophic conditions also included shifts between the grazing chain (which include large predators, e.g., piscivorous fish, mammals, and birds at the top of the food chain) and the microbial loop (filtering top predators such as jellyfish). Another large-scale change has been a succession from low (freshwater glacier lake) biodiversity to increased (brackish and marine) biodiversity. The present-day Baltic Sea ecosystem is a direct descendant of the more marine Litorina Sea, which marks the beginning of the transition from a primeval ecosystem to one regulated by humans. The recent Baltic Sea is characterized by high concentrations of pollutants and nutrients, a shift from perennial to annual macrophytes (and more rapid nutrient cycling), and an increasing rate of invasion by non-native species. Thus, an increasing pace of anthropogenic ecological change has been a prominent trend in the Baltic Sea ecosystem since the Ancylus Lake.Future development is in the first place dependent on regional factors, such as salinity, which is regulated by sea and land level changes and the climate, and runoff, which controls both salinity and the leaching of nutrients to the sea. However, uncertainties abound, for example the future development of the Gulf Stream and its associated westerly winds, which support the sub-boreal ecosystems, both terrestrial and aquatic, in the Baltic Sea area. Thus, extensive sophisticated, cross-disciplinary modeling is needed to foresee whether the Baltic Sea will develop toward a freshwater or marine ecosystem, set in a sub-boreal, boreal, or arctic climate.

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