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1

De Pascale, Stefania, Francesco Orsini, Rosanna Caputo, Maria Antonella Palermo, Giancarlo Barbieri, and Albino Maggio. "Seasonal and multiannual effects of salinisation on tomato yield and fruit quality." Functional Plant Biology 39, no. 8 (2012): 689. http://dx.doi.org/10.1071/fp12152.

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The effects of short- and long-term salinisation were studied by comparing tomato growth on a soil exposed to one-season salinisation (short term) vs growth on a soil exposed to >20 years salinisation (long term). Remarkable differences were associated to substantial modifications of the soil physical-chemical characteristics in the root zone, including deteriorated structure, reduced infiltration properties and increased pH. Fresh yield, fruit number and fruit weight were similarly affected by short- and long-term salinisation. In contrast, the marketable yield was significantly lower in t
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Qin, Ziyuan, Tangzhe Nie, Ying Wang, et al. "The Characteristics and Driving Factors of Soil Salinisation in the Irrigated Area on the Southern Bank of the Yellow River in Inner Mongolia: A Assessment of the Donghaixin Irrigation District." Agriculture 15, no. 5 (2025): 566. https://doi.org/10.3390/agriculture15050566.

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Soil salinisation is a critical problem in northern China’s arid and semi-arid irrigated regions, posing a substantial impediment to the sustainable advancement of agriculture in these areas. This research utilises the Donghaixin Irrigation District, located on the southern bank of the Yellow River in Inner Mongolia, as a case study. This study examines the spatial distribution and determinants of soil salinisation through macro-environmental variables and micro-ion composition, integrating regression models and groundwater ion characteristics to elucidate the patterns and causes of soil salin
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3

Schulz, Claus-Jürgen. "Salinisation of running waters." Limnologica 41, no. 2 (2011): 79. http://dx.doi.org/10.1016/j.limno.2011.01.003.

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4

Hoey, D., M. Ahmed, and M. Littleboy. "Landscape Salinisation and Management: An Australian Perspective." Journal of Agricultural and Marine Sciences [JAMS] 7, no. 2 (2002): 53. http://dx.doi.org/10.24200/jams.vol7iss2pp53-60.

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Australian landscapes are facing an increasing salinisation threat. It is estimated that 2.5 million hectares are affected by land salinisation, and this area is expected to triple by 2050. Federal and State governments have jointly developed a policy framework to address this issue, with each state refining their own salinity management strategies within this framework. Scientific assessment and modelling underpin these salinity management strategies, though socio-economic considerations are also important. Landscape salinity assessment techniques used in the Australian context are outlined,
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5

Chabab, Elena, Michael Kühn, and Thomas Kempka. "Upwelling mechanisms of deep saline waters via Quaternary erosion windows considering varying hydrogeological boundary conditions." Advances in Geosciences 58 (November 14, 2022): 47–54. http://dx.doi.org/10.5194/adgeo-58-47-2022.

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Abstract. Intrusion of deep saline waters into freshwater aquifers does not only endanger the regional drinking water supply, but also rivers and stagnant waters and their fauna are threatened by salinisation. The upwelling of highly mineralised saline waters in large parts of the North German Basin is favoured by the presence of Elsterian glacial erosion windows in the Lower Oligocene Rupelian Clay, the most important hydraulic confining unit in this region. Lower precipitation rates and decreasing groundwater levels as a consequence of global climate change, but also anthropogenic interventi
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6

Pauw, P., P. G. B. de Louw, and G. H. P. Oude Essink. "Groundwater salinisation in the Wadden Sea area of the Netherlands: quantifying the effects of climate change, sea-level rise and anthropogenic interferences." Netherlands Journal of Geosciences - Geologie en Mijnbouw 91, no. 3 (2012): 373–83. http://dx.doi.org/10.1017/s0016774600000500.

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AbstractHydrogeological research in coastal areas has gained considerable attention over the last decades due to increasing stresses on fresh groundwater resources. Fundamental groundwater flow and solute transport analyses remain essential for a concise understanding of the governing processes that lead to salinisation of fresh groundwater resources. However, the challenge of modern research is the application and quantification of these processes in real world cases. In this context, deltaic areas are amongst the most difficult study areas as they often have a complex groundwater salinity di
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7

Tillner, Elena, Maria Langer, Thomas Kempka, and Michael Kühn. "Fault damage zone volume and initial salinity distribution determine intensity of shallow aquifer salinisation in subsurface storage." Hydrology and Earth System Sciences 20, no. 3 (2016): 1049–67. http://dx.doi.org/10.5194/hess-20-1049-2016.

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Abstract. Injection of fluids into deep saline aquifers causes a pore pressure increase in the storage formation, and thus displacement of resident brine. Via hydraulically conductive faults, brine may migrate upwards into shallower aquifers and lead to unwanted salinisation of potable groundwater resources. In the present study, we investigated different scenarios for a potential storage site in the Northeast German Basin using a three-dimensional (3-D) regional-scale model that includes four major fault zones. The focus was on assessing the impact of fault length and the effect of a secondar
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8

Snezhko, V. L., D. M. Benin, and N. V. Gavrilovskaya. "Salinisation of Reclaimed Agricultural Land in the Altai Territory: Cluster Analysis." Timiryazev Biological Journal, no. 2 (March 21, 2023): 107–17. http://dx.doi.org/10.26897/2949-4710-2023-2-107-117.

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The Altai Territory occupies a leading position among the constituent entities of the Siberian Federal District in terms of arable land, of which more than 80% are located in the zone of unstable moisture. Irrigation is the predominant form of agricultural hydraulic reclamation in the region. The area of irrigated land is about 69 thousand hectares, of which almost 10% of the area has varying degrees of salinity in the 0‑100 cm layer. Prolonged irrigation and non-compliance with irrigation technologies can lead to salinisation of land. In the Russian Federation, all irrigation systems havecomm
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9

Wilkinson, Kate, Tessa Chamberlain, and Mike Grundy. "Investigation into salinisation in southwestern Queensland." ASEG Extended Abstracts 2004, no. 1 (2004): 1–4. http://dx.doi.org/10.1071/aseg2004ab159.

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10

Barnett, Steve. "The looming threat of aquifer salinisation." ASEG Extended Abstracts 2006, no. 1 (2006): 1–4. http://dx.doi.org/10.1071/aseg2006ab009.

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11

Jiang, Shan, Xuan Wu, Sichan Du, Qin Wang, and Dawei Han. "Are UK Rivers Getting Saltier and More Alkaline?" Water 14, no. 18 (2022): 2813. http://dx.doi.org/10.3390/w14182813.

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River salinisation and alkalinisation have become one of the major environmental problems threatening the safety of global freshwater resources. With the accelerated climate change and aggravating anthropogenic influences, it is important to identify the trends and causes of river salinisation and alkalinisation so that better mitigation measures could be taken. This study has focused on the UK rivers because there has been insufficient investigation on this topic. To understand the salinisation and alkalinisation trends and causes of rivers in the UK over the past 20 years from a vertical (an
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12

Armour, RJ, and MF Viljoen. "An economic case for drainage for sustainable irrigation: Case studies in the lower Vaal and Riet catchments." South African Journal of Economic and Management Sciences 10, no. 4 (2014): 470–81. http://dx.doi.org/10.4102/sajems.v10i4.1060.

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Where evaporation exceeds precipitation salinisation is inevitable. This paper presents a multidisciplinary framework of the dynamic interactions between the hydrology, bio-physical and economics of irrigated agriculture in a semi arid area. Status quo drainage and cropping situations are compared to a scenario of increased drainage and leaching and subsequent higher value crops. Stochastically generated hydrology data fitted to a salinisation:yield production function is inputted in a crop enterprise budget (CEB) simulation model.Results show losses due to salinisation of up to R6 962/ha, whi
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13

Akeroyd, M. D., G. R. Walker, and M. B. Kendall. "Response of Eucalyptus largiflorens to floodplain salinisation." Water Science and Technology 48, no. 7 (2003): 113–20. http://dx.doi.org/10.2166/wst.2003.0431.

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An analysis of the stable isotopes from the tree rings of Eucalyptus largiflorens on the Chowilla Floodplain was undertaken. This chronology of tree water use responses was compared to the known hydrological changes that have occurred due to the effects of river regulation. The isotope chronology indicates that E. largiflorens has always oscillated between groundwater and rain-derived soil water and river regulation has apparently had little effect on tree water sources over time. This result is surprising, but no doubt reflects the complexity of floodplain processes and interactions between t
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14

Cañedo-Argüelles, Miguel, Ben J. Kefford, Christophe Piscart, Narcís Prat, Ralf B. Schäfer, and Claus-Jürgen Schulz. "Salinisation of rivers: An urgent ecological issue." Environmental Pollution 173 (February 2013): 157–67. http://dx.doi.org/10.1016/j.envpol.2012.10.011.

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15

González, Esther M. "Drought Stress Tolerance in Plants." International Journal of Molecular Sciences 24, no. 7 (2023): 6562. http://dx.doi.org/10.3390/ijms24076562.

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16

Florinsky, I. V., R. G. Eilers, and G. W. Lelyk. "Prediction of soil salinity risk by digital terrain modeling in the Canadian prairies." Canadian Journal of Soil Science 80, no. 3 (2000): 455–63. http://dx.doi.org/10.4141/s99-093.

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Soil salinisation is a typical problem for the Canadian prairies. At macro-topographic scale, build-up of salts occurs in depressions. However, this relationship is not displayed on existing small-scale maps of soil salinity. To improve these maps, one can use a concept of accumulation, transition and dissipation zones of the landsurface. The concept allows one to reveal depressions (topographically expressed accumulation zones) using digital models of horizontal and vertical curvatures, or accumulation and mean curvatures derived from a digital elevation model. We applied the concept of accum
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17

Beatty, Stephen J., David L. Morgan, Mahmoud Rashnavadi, and Alan J. Lymbery. "Salinity tolerances of endemic freshwater fishes of south-western Australia: implications for conservation in a biodiversity hotspot." Marine and Freshwater Research 62, no. 1 (2011): 91. http://dx.doi.org/10.1071/mf10100.

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Secondary salinisation represents an important threat to terrestrial and aquatic habitats throughout the world. In south-western Australia, widespread salinisation of waterways has caused large range reductions in the highly endemic freshwater fish fauna. We hypothesised that differences in the distributions of three fish species within the salinised Blackwood River would be related to their salinity tolerances. Galaxias occidentalis was widespread throughout the catchment, whereas Nannoperca vittata was restricted to the main channel and freshwater tributaries of the lower catchment, and Nann
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18

Demba DIONE, Ibrahima, Abdou KA, Fatoumata HANE, et al. "INSULARITY, ENVIRONMENTAL VULNERABILITIES AND ADAPTATION STRATEGIES IN THE BLISS KASSA ISLANDS IN CASAMANCE (SENEGAL)." International Journal of Advanced Research 12, no. 08 (2024): 145–56. http://dx.doi.org/10.21474/ijar01/19237.

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The relationship between the environment and societies is a complex one in terms of the way in which human communities interact with the environment. This relationship is characteristic of the different uses made of the areas in which they live. A segmented approach is therefore needed to understand how these areas are changing, hence the choice in this research to focus on small island areas in the Ziguinchor region of southern Senegal. The article looks at three main challenges identified in this area, including waste production and management, sea encroachment and salinisation. A qualitativ
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19

Sene, François Ngor, Aïdara C. A. Lamine Fall, and Yancouba Sane. "Dégradation des Terres Agricoles par Salinisation dans la Vallée Fossile du Sine : Cas de la Commune de Niakhar (Région de Fatick)." European Scientific Journal, ESJ 20, no. 35 (2024): 142. https://doi.org/10.19044/esj.2024.v20n35p142.

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La salinisation des terres, phénomène mondial qui affecte particulièrement les zones sous influence fluviomarine, constitue une contrainte majeure pour l’agriculture. Cette étude vise à comprendre le processus de dégradation des terres agricoles par salinisation dans la vallée fossile du Sine, notamment dans la commune de Niakhar, région de Fatick. En combinant l’analyse de la conductivité électrique des sols, la cartographie basée sur des indices de télédétection (NDSI, SI, BI et ISN issus des images Landsat 7 et 8) et des enquêtes socioéconomiques, les résultats montrent que la salinisation
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20

Jana, Atashi, and Gouri Sankar Bhunia. "Vegetation Cover Analysis Based on NDVI in Moushuni Island, Sundarban, India." International Journal for Research in Applied Science and Engineering Technology 10, no. 5 (2022): 2669–74. http://dx.doi.org/10.22214/ijraset.2022.42883.

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Abstract: Moushuni island is one of the island of Indian Sundarban, but changes of vegetation cover is occurred due to natural and anthropogenic activity. The aim of this paper is to emphasis the changes of vegetation cover between 2000 and 2020 of Moushuni island. Vegetation indices like Normalised Difference Vegetation Index (NDVI) is used to identify the changes of vegetation cover from 2000 to 2020. Based on NDVI value, the study area is classified into four classes -Dense vegetation, Sparse Vegetation(vegetated), No vegetation and Water. Result shows an overall increase of dense vegetatio
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21

Kijne, J. W. "Salinisation in irrigated agriculture in Pakistan: mistaken predictions." Water Policy 8, no. 4 (2006): 325–38. http://dx.doi.org/10.2166/wp.2006.045.

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This paper revisits data and information that was collected through field studies by the International Irrigation Management Institute (IIMI) in Pakistan in the early 1990s. Analysis of available data led in 1996 to the publication of an IIMI research report (Kijne, 1996) whose main conclusion was that current cropping intensities and groundwater usage in Pakistan's irrigated agriculture were not sustainable. Ten years on there is no evidence that this prediction came true and the paper questions why those predictions were wrong. Based on more recent field data and information, the water and s
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Grujić, Gordana, Jovica Vasin, and Milivoj Belić. "Soil salinisation in Vojvodina - the Republic of Serbia." Current Opinion in Environmental Sustainability 50 (June 2021): 149–58. http://dx.doi.org/10.1016/j.cosust.2021.03.015.

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23

Dehaan, R., and G. R. Taylor. "Image-derived spectral endmembers as indicators of salinisation." International Journal of Remote Sensing 24, no. 4 (2003): 775–94. http://dx.doi.org/10.1080/01431160110107635.

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24

Abdelhafid, Youcef, Miled Zohra Rechachi, and Amor Halitim. "Caractérisation géochimique des eaux d’irrigation de la palmeraie d’Oumache (oasis des Ziban, sud-est de l’Algérie)." Revue des sciences de l’eau 32, no. 1 (2019): 69–81. http://dx.doi.org/10.7202/1059881ar.

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Résumé L’ancienne palmeraie d’Oumache située à l’aval de Zab el Gharbi (ouest de Ziban-Biskra, sud-est de l’Algérie) connait aujourd'hui un déclin dû essentiellement à l’insuffisance de l’eau d’irrigation et à la remontée des eaux trop chargées de la nappe phréatique. De plus, le milieu endoréique très évaporant a accéléré le phénomène de salinisation du sol. Ce travail traite de la caractérisation géochimique des eaux (forage et nappe) utilisées pour l’irrigation en vue d’une meilleure gestion de l’irrigation. Les résultats montrent que l’eau de forage présente un risque élevé de salinisation
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25

Claros, Manuel Gonzalo, Amanda Bullones, Antonio Jesús Castro, et al. "Multi-Omic Advances in Olive Tree (Olea europaea subsp. europaea L.) Under Salinity: Stepping Towards ‘Smart Oliviculture’." Biology 14, no. 3 (2025): 287. https://doi.org/10.3390/biology14030287.

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Soil salinisation is threatening crop sustainability worldwide, mainly due to anthropogenic climate change. Molecular mechanisms developed to counteract salinity have been intensely studied in model plants. Nevertheless, the economically relevant olive tree (Olea europaea subsp. europaea L.), being highly exposed to soil salinisation, deserves a specific review to extract the recent genomic advances that support the known morphological and biochemical mechanisms that make it a relative salt-tolerant crop. A comprehensive list of 98 olive cultivars classified by salt tolerance is provided, toge
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El Bastawesy, M., and R. Ramadan Ali. "The use of GIS and remote sensing for the assessment of waterlogging in the dryland irrigated catchments of Farafra Oasis in Egypt." Hydrology and Earth System Sciences Discussions 8, no. 6 (2011): 10535–63. http://dx.doi.org/10.5194/hessd-8-10535-2011.

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Abstract. This paper investigates the interplay of the hydrogeological characteristics, soil properties and recent land reclamation projects on the distribution of waterlogging and salinisation within the Farafra Oasis. The multi-temporal remote sensing data and field observations show that new reclaimed areas have been recently cultivated in distant areas from the old agricultural land. These new cultivations have developed widespread water logging, seepage channels and soil salinisation. Analyses of the Shuttle Radar Topography Mission (SRTM) Digital Elevation Model (DEM) showed that both ol
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Cunillera-Montcusí, David, Meryem Beklioğlu, Miguel Cañedo-Argüelles, et al. "Freshwater salinisation: a research agenda for a saltier world." Trends in Ecology & Evolution 37, no. 5 (2022): 440–53. http://dx.doi.org/10.1016/j.tree.2021.12.005.

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28

Howlett, A., M. J. Roach, and J. E. Reid. "Geophysical Characteristics of Salinisation at Cape Portland, NE Tasmania." ASEG Extended Abstracts 2001, no. 1 (2001): 1–4. http://dx.doi.org/10.1071/aseg2001ab058.

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Howlett, A., M. J. Roach, and J. E. Reid. "Geophysical Characteristics of Salinisation at Cape Portland, NE Tasmania." Exploration Geophysics 32, no. 3-4 (2001): 214–18. http://dx.doi.org/10.1071/eg01214.

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30

Schofield, N. J., and J. K. Ruprecht. "Regional analysis of stream salinisation in southwest Western Australia." Journal of Hydrology 112, no. 1-2 (1989): 19–39. http://dx.doi.org/10.1016/0022-1694(89)90178-9.

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31

Ghassemi, F., A. J. Jakeman, and H. A. Nix. "Human induced salinisation and the use of quantitative methods." Environment International 17, no. 6 (1991): 581–94. http://dx.doi.org/10.1016/0160-4120(91)90170-u.

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32

Ruprecht, John, Tim Sparks, Ning Liu, Bernard Dell, and Richard Harper. "Using reforestation to reverse salinisation in a large watershed." Journal of Hydrology 577 (October 2019): 123976. http://dx.doi.org/10.1016/j.jhydrol.2019.123976.

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33

Feitz, Andrew J., and Sven Lundie. "Soil salinisation: a local life cycle assessment impact category." International Journal of Life Cycle Assessment 7, no. 4 (2002): 244–49. http://dx.doi.org/10.1007/bf02978880.

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34

Kuzmenko, Eduard, Serhiy Bagriy, Ihor Chepurnyi, and Tetiana Chepurna. "Monitoring studies of the ecological and hydrogeochemical situation in the zone of influence of technogenic objects of the mining and industrial complex of the Kalush-Holyn Potash Deposit." Ecological Safety and Balanced Use of Resources 10, no. 4 (2024): 83–85. https://doi.org/10.69628/esbur/2.2024.83.

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The assessment of groundwater and surface water conditions in areas of depleted salt deposits is a crucial component of monitoring studies due to the significant anthropogenic impact of objects such as tailings ponds, sludge accumulators, and the Dombrovskyi Quarry. The aim of the study was to establish, based on real experimental data from hydrogeochemical analyses of long-term groundwater monitoring via a network of hydrogeological observation wells, the areas of groundwater salinisation in the Kalush mining and industrial region, to assess the dynamics of chemical and physico-chemical indic
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35

Huynh, Thu. "Potential in enhancement of salinity tolerance to crops in Vietnam’s Mekong Delta using endophytes: A review." IOP Conference Series: Earth and Environmental Science 1340, no. 1 (2024): 012026. http://dx.doi.org/10.1088/1755-1315/1340/1/012026.

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Abstract Mekong Delta is the most important agricultural area of Vietnam. In the backdrop of recent climate change, the salinisation in soil is threatening crop plants causing serious damages such as yield loss as well as inhibition of crop quality and productivity in the region. Under salinisation conditions, plant growth and development have to experience negative effects to adverse conditions. The high concentration of Na+ ions in plants hampers water and nutrient uptakes, inhibits pathway of photosynthesis, and changes physiological and molecular mechanisms causing intracellular osmotic an
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Mouatassime Sabri, El, Ahmed Boukdir, Ismail Karaoui, Abdelkrim Arioua, Rachid Messlouhi, and Abdelkhalek El Amrani Idrissi. "Modelling soil salinity in Oued El Abid watershed, Morocco." E3S Web of Conferences 37 (2018): 04002. http://dx.doi.org/10.1051/e3sconf/20183704002.

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Soil salinisation is a phenomenon considered to be a real threat to natural resources in semi-arid climates. The phenomenon is controlled by soil (texture, depth, slope etc.), anthropogenic factors (drainage system, irrigation, crops types, etc.), and climate factors. This study was conducted in the watershed of Oued El Abid in the region of Beni Mellal-Khenifra, aimed at localising saline soil using remote sensing and a regression model. The spectral indices were extracted from Landsat imagery (30 m resolution). A linear correlation of electrical conductivity, which was calculated based on so
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Wedderburn, Scotte D., Keith F. Walker, and Brenton P. Zampatti. "Salinity may cause fragmentation of hardyhead (Teleostei: Atherinidae) populations in the River Murray, Australia." Marine and Freshwater Research 59, no. 3 (2008): 254. http://dx.doi.org/10.1071/mf07205.

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Salinisation in lowland areas of the Murray–Darling Basin, Australia, has had noticeable effects on fish. The endangered endemic Murray hardyhead Craterocephalus fluviatilis is distributed patchily and confined mainly to saline waters (0.4–20 g L–1), whereas the unspecked hardyhead C. stercusmuscarum fulvus has a more continuous distribution but is absent from high salinities (>10). Osmoregulation was compared in these two congeners and an estuarine atherinid, the small-mouth hardyhead Atherinosoma microstoma, over a wide salinity range (0.03–85). All three species are euryhaline, although
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Amzallag, G. Nissim. "Influence of Periodic Fluctuations in Root Environment on Adaptation to Salinity in Sorghum bicolor." Functional Plant Biology 24, no. 5 (1997): 579. http://dx.doi.org/10.1071/pp96018.

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In Sorghum bicolor (L.) Moench, a 3-week exposure to 75 mM NaCl induced the ability to grow at 300 mm NaCl, a lethal concentration for non-pretreated plants. This property was defined as adaptation to salinity. The chemical composition of the root medium was periodically modified during the 3-week maturation of the adaptation response. Two daily 1-h interruptions of the salinisation treatment were sufficient to prevent the initiation of the adaptation process, while two daily 1-h modifications of the external NaCl concentration only disturbed its completion. Moreover, the effect of a short int
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Andreeva, Nataliya. "Determination of Magnesium Salinity in Belozem Region, Bulgaria." Bulgarian Journal of Soil Science 5, no. 1 (2020): 11–22. https://doi.org/10.5281/zenodo.3865412.

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Salinisation is an important soil-forming process (primary or secondary), characterized by an excess of water-soluble salts and/or exchangeable sodium. The amount of exchangeable magnesium is also essential for the more detailed determination of the physico-chemical properties of saline soils. The determination of magnesium salinity is still a debatable issue, but there are already criteria in the literature for its estimation. The Belozem region is representative of Bulgaria for the processes of alkaline salinisation, but the presence and extent of magnesium salinity has not been determined.
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Bak, Malgorzata, Dariusz Halabowski, Adrian Kryk, Iga Lewin, and Agnieszka Sowa. "Mining salinisation of rivers: its impact on diatom (Bacillariophyta) assemblages." Fottea 20, no. 1 (2020): 1–16. http://dx.doi.org/10.5507/fot.2019.010.

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41

Khayrulina, Elena, Anna Bogush, Larisa Novoselova, and Natalya Mitrakova. "Properties of Alluvial Soils of Taiga Forest under Anthropogenic Salinisation." Forests 12, no. 3 (2021): 321. http://dx.doi.org/10.3390/f12030321.

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The environmental impact of deposit development can be indirect and can cause combined geochemical processes in ecosystems. These must be taken into consideration under environmental forecasting and environmental risk assessment. Soil degradation in the Taiga Forest is considered, within the area of Verkhnekamskoye potash deposit (Russia), as an example of such environmental transformation. Here, the mechanism and characteristics of the anthropogenic salinisation of alluvial soils under potash deposit development are newly described. It was found that there is a strong anthropogenic impact of
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42

Wilkinson, Kate, Tessa Chamberlain, and Mike Grundy. "The role of geophysics in understanding salinisation in Southwestern Queensland." BUTSURI-TANSA(Geophysical Exploration) 58, no. 1 (2005): 78–85. http://dx.doi.org/10.3124/segj.58.78.

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43

Wilkinson, Kate, Tessa Chamberlain, and Mike Grundy. "The role of geophysics in understanding salinisation in Southwestern Queensland." Exploration Geophysics 36, no. 1 (2005): 78–85. http://dx.doi.org/10.1071/eg05078.

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44

Jacobson, Gerry. "Guest Editor’s Preface: Groundwater processes in land and water salinisation." Hydrogeology Journal 5, no. 1 (1997): 4–5. http://dx.doi.org/10.1007/s10040-997-0009-z.

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45

Mausbach, William E., and Andrew R. Dzialowski. "Salinisation reduces biodiversity in neighbouring freshwater patches in experimental metacommunities." Freshwater Biology 65, no. 3 (2019): 592–604. http://dx.doi.org/10.1111/fwb.13457.

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46

Kašovská, Kamila, Łukasz Pierzchała, Edyta Sierka, and Barbara Stalmachová. "Impact of the Salinity Gradient on the Mollusc Fauna in Flooded Mine Subsidences (Karvina, Czech Republic)." Archives of Environmental Protection 40, no. 1 (2014): 87–99. http://dx.doi.org/10.2478/aep-2014-0007.

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Abstract This paper presents the impact of salinisation on the aquatic mollusc fauna in flooded mine subsidences in the Karvina region (Czech Republic). The results of the previous research on salinity in flooded mine subsidences show that some of them contain a high content of dissolved inorganic substances (above 1000 mg·l-1). These substances can affect the vegetation and animals occurring in the water and the surrounding area. The phylum of Mollusca was selected as a model group for the fieldwork as it includes species with the proven bioindication potential. The occurrence of aquatic moll
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47

Jiang, Jinyuan, Huibin Yu, Beidou Xi, Fansheng Meng, Yuexi Zhou, and Hongliang Liu. "UV - visible spectroscopic properties of dissolved fulvic acids extracted from salined fluvo-aquic soils in the Hetao Irrigation District, China." Soil Research 49, no. 8 (2011): 670. http://dx.doi.org/10.1071/sr11213.

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The elemental composition and the UV–visible spectroscopic properties of dissolved fulvic acids (FA) extracted from salined fluvo-aquic soils in the Hetao Irrigation District were examined to evaluate the humification degree of FA and salinisation processes of soils. Composite soil samples of different depths (0–20, 20–40, 40–60, 60–80 cm) were collected from four native halophyte soils [communities Salicornia europaea (CSE), Suaeda glauca (CSG), Kalidium foliatum (CKF), Sophora alopecuroides (CSA)] and two furrow-irrigated fields [corn (CFD), wheat (WFD)] along a saline impact gradient. Seven
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48

Bethune, Matthew. "Towards effective control of deep drainage under border-check irrigated pasture in the Murray-Darling Basin: a review." Australian Journal of Agricultural Research 55, no. 5 (2004): 485. http://dx.doi.org/10.1071/ar03192.

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High watertables and land salinisation threaten the sustainability and prosperity of the irrigated dairy industry in the Murray–Darling Basin of Australia. High watertables and salinisation result from excessive deep drainage. Spatial and temporal trends in deep drainage data pertinent to the dairy industry in the Murray–Darling Basin are reviewed with a view towards reducing deep drainage. The reviewed data indicate that deep drainage under border-check irrigated pasture is generally greater than the leaching requirement and can be reduced without affecting pasture growth. Deep drainage throu
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George, Richard, Jonathan Clarke, and Pauline English. "Modern and palaeogeographic trends in the salinisation of the Western Australian wheatbelt: a review." Soil Research 46, no. 8 (2008): 751. http://dx.doi.org/10.1071/sr08066.

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The Western Australian wheatbelt contains vast areas of agricultural land underlayed by saline and deeply weathered regolith derived from Archaean rocks and recent sediments. The region has been geologically stable since the late Permian, although the Archaean basement sustained some movement during the break-up of Gondwanaland and the northward drift of Australia from Antarctica. During the Early Cretaceous, Eocene and more recently, the wheatbelt region’s weathered mantle has been successively eroded by rivers. The palaeovalleys have been infilled with terrestrial and marine sediments, and s
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Overton, I. C., I. D. Jolly, P. G. Slavich, M. M. Lewis, and G. R. Walker. "Modelling vegetation health from the interaction of saline groundwater and flooding on the Chowilla floodplain, South Australia." Australian Journal of Botany 54, no. 2 (2006): 207. http://dx.doi.org/10.1071/bt05020.

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The native riparian vegetation communities on the Chowilla floodplain in the lower River Murray in South Australia are suffering severe declines in health, particularly the Eucalyptus camaldulensis Dehnh. (red gum) and Eucalyptus largiflorens F.Muell. (black box) communities. The primary cause of the decline is salinisation of the floodplain soils caused by increased rates of groundwater discharge and hence increased movement of salt up into the plant root zone. The salinity is driven by a lack of flooding and rising saline groundwater tables. Rises in the naturally saline groundwater levels a
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