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| Author | Kisi, O.; Ardiçlio\uglu, M.; Hadi, A.M.W.; Kuriqi, A.; Kulls, C. | ||||
| Title | Estimation of mean velocity upstream and downstream of a bridge model using metaheuristic regression methods | Type | Journal Article | ||
| Year | 2023 | Publication | Water Resources Management | Abbreviated Journal | |
| Volume | 37 | Issue  |
14 | Pages | 5559-5580 |
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| Publisher | Springer Netherlands Dordrecht | Place of Publication | Editor | ||
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| Notes | Approved | no | |||
| Call Number | THL @ christoph.kuells @ kisi2023estimation | Serial | 223 | ||
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| Author | Glavas, S.; Moschonas, N. | ||||
| Title | Origin of observed acidic–alkaline rains in a wet-only precipitation study in a Mediterranean coastal site, Patras, Greece | Type | Journal Article | ||
| Year | 2002 | Publication | Atmospheric Environment | Abbreviated Journal | |
| Volume | 36 | Issue |
19 | Pages | 3089-3099 |
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| Publisher | Elsevier | Place of Publication | Editor | ||
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| Notes | Approved | no | |||
| Call Number | THL @ luqianxue.zhang @ glavas2002origin | Serial | 91 | ||
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| Author | Pezzarossa, B.; Piccotino, D.; Petruzzelli, G. | ||||
| Title | Sorption and desorption of selenium in different soils of the Mediterranean area | Type | Journal Article | ||
| Year | 1999 | Publication | Communications in soil science and plant analysis | Abbreviated Journal | |
| Volume | 30 | Issue |
19-20 | Pages | 2669-2679 |
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| Publisher | Taylor & Francis | Place of Publication | Editor | ||
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| Notes | Approved | no | |||
| Call Number | THL @ luqianxue.zhang @ pezzarossa1999sorption | Serial | 76 | ||
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| Author | Hanshaw, B.B.; Back, W. | ||||
| Title | Deciphering hydrological systems by means of geochemical processes | Type | Journal Article | ||
| Year | 1985 | Publication | Hydrological Sciences Journal | Abbreviated Journal | |
| Volume | 30 | Issue |
2 | Pages | 257-271 |
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| Abstract | The distribution of permeability and chemical character of groundwater in carbonate aquifers is significantly influenced by the many diagenetic processes and reactions that occur in the early development of these rocks. Many of these diagenetic processes occur in the transition zone formed as the carbonate sediments emerge from the marine environment and become fresh-water aquifers. Analyses of trace elements and isotopes indicate that calcite cements and dolomites are formed in this groundwater mixing zone. Reverse reactions such as mineral dissolution and dedolomitization occur in carbonate aquifer systems. The geochemical reactivity of the fresh-water/salt-water mixing zone results from the nonlinearity of geochemical parameters as a function of ionic strength and causes extensive dissolution in coastal carbonate rocks. Interpretation of geochemical reactions and isotopic composition of groundwater provides a method to determine hydrological parameters such as porosity, hydraulic conductivity, and groundwater flow rates. This geochemical method is largely independent of the more conventional approach of determining these parameters by an evaluation of physical properties of aquifer systems. |
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| ISSN | 0262-6667 | ISBN | Medium | ||
| Area | Expedition | Conference | |||
| Notes | Approved | no | |||
| Call Number | THL @ christoph.kuells @ Hanshaw1985 | Serial | 25 | ||
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| Author | de Paz, J.-M.; Sánchez, J.; Visconti, F. | ||||
| Title | Combined use of GIS and environmental indicators for assessment of chemical, physical and biological soil degradation in a Spanish Mediterranean region | Type | Journal Article | ||
| Year | 2006 | Publication | Journal of environmental management | Abbreviated Journal | |
| Volume | 79 | Issue |
2 | Pages | 150-162 |
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| Abstract | Soil is one of the main non-renewable natural resources in the world. In the Valencian Community (Mediterranean coast of Spain), it is especially important because agriculture and forest biomass exploitation are two of the main economic activities in the region. More than 44% of the total area is under agriculture and 52% is forested. The frequently arid or semi-arid climate with rainfall concentrated in few events, usually in the autumn and spring, scarcity of vegetation cover, and eroded and shallow soils in several areas lead to soil degradation processes. These processes, mainly water erosion and salinization, can be intense in many locations within the Valencian Community. Evaluation of soil degradation on a regional scale is important because degradation is incompatible with sustainable development. Policy makers involved in land use planning require tools to evaluate soil degradation so they can go on to develop measures aimed at protecting and conserving soils. In this study, a methodology to evaluate physical, chemical and biological soil degradation in a GIS-based approach was developed for the Valencian Community on a 1/200,000 scale. The information used in this study was obtained from two different sources: (i) a soil survey with more than 850 soil profiles sampled within the Valencian Community, and (ii) the environmental information implemented in the Geo-scientific map of the Valencian Community digitised on an Arc/Info GIS. Maps of physical, chemical and biological soil degradation in the Valencian Community on a 1/200,000 scale were obtained using the methodology devised. These maps can be used to make a cost-effective evaluation of soil degradation on a regional scale. Around 29% of the area corresponding to the Valencian Community is affected by high to very high physical soil degradation, 36% by high to very high biological degradation, and 6% by high to very high chemical degradation. It is, therefore, necessary to draw up legislation and to establish the policy framework for actions focused on preventing soil degradation and conserving its productive potential. |
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| Publisher | Elsevier | Place of Publication | Editor | ||
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| ISSN | 0301-4797 | ISBN | Medium | ||
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| Notes | Approved | no | |||
| Call Number | THL @ luqianxue.zhang @ dePaz2006 | Serial | 47 | ||
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