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Chapter 1 occurrence of groundwater
Chapter 1 occurrence of groundwater
Usama Waly
Aquifer Parameter Estimation
Aquifer Parameter Estimation
C. P. Kumar
Water Resources Engineering
Aquifers
Aquifers
Tarun kumar
After attending this module, the user would be able to know about the most popular methods of groundwater exploration.
Groundwater exploration methods
Groundwater exploration methods
Prof. A.Balasubramanian
This module explains about the water-bearing geological formations called as aquifers and their types.
Aquifer types
Aquifer types
Prof. A.Balasubramanian
It includes the definition, properties, classification of groundwater with appropriate examples and figures in details. It also deals about the formation of groundwater. The properties of aquifers (all of 7) are described here in details with figures and mathematical terms.
Groundwater Properties
Groundwater Properties
Minhaz Hasan
Detailed ppt on different types of aquifers: aquifer, aquitard, aquiclude, aquifuge
Types of Aquifers
Types of Aquifers
Ananya21Mittal
Over the last decade, demand for spring management has increased as traditional spring sources have started drying up or becoming contaminated. In response, communities, NGOs and state agencies began dedicated spring protection programmes. In the Himalayas, the State of Sikkim and organizations such as Central Himalayan Action and Research Group (CHIRAG) and People Science Institute (PSI) started identifying and protecting spring recharge areas around 2007. The difference between these programmes and many other previous efforts is that they went beyond supply-side improvements to focus on the use of hydrogeology to map springsheds for targeted interventions. The Advanced Centre for Water Resources Development and Management (ACWADAM), a research and capacity-building organization comprised of hydrogeologists and other experts began lending their expertise and building capacity of stakeholders. ACWADAM provides technical support, training and materials in hydrogeology to all network partners as well as others in India and the region. Similar programmes began independently in most of the mountain regions of India. Arghyam, a funding organization that was supporting many of these programmes, noticed that these disparate initiatives shared commonalities despite geographic diversity. They thus organized and funded a meeting of these various organizations in June 2014, and the Springs Initiative was born. The springs initiative aims to tackle the current water crisis and to ensure safe and sustainable access to water for all, by promoting responsible and appropriate management of aquifers, springsheds, and watersheds and conserving ecosystems in partnership with communities, governments and other stakeholders. This presentation has been developed as a part of the springs initiative to promote an understanding of springs and their role in mountainous areas.
Spring hydrogeology and its classification
Spring hydrogeology and its classification
India Water Portal
Recommandé
Chapter 1 occurrence of groundwater
Chapter 1 occurrence of groundwater
Usama Waly
Aquifer Parameter Estimation
Aquifer Parameter Estimation
C. P. Kumar
Water Resources Engineering
Aquifers
Aquifers
Tarun kumar
After attending this module, the user would be able to know about the most popular methods of groundwater exploration.
Groundwater exploration methods
Groundwater exploration methods
Prof. A.Balasubramanian
This module explains about the water-bearing geological formations called as aquifers and their types.
Aquifer types
Aquifer types
Prof. A.Balasubramanian
It includes the definition, properties, classification of groundwater with appropriate examples and figures in details. It also deals about the formation of groundwater. The properties of aquifers (all of 7) are described here in details with figures and mathematical terms.
Groundwater Properties
Groundwater Properties
Minhaz Hasan
Detailed ppt on different types of aquifers: aquifer, aquitard, aquiclude, aquifuge
Types of Aquifers
Types of Aquifers
Ananya21Mittal
Over the last decade, demand for spring management has increased as traditional spring sources have started drying up or becoming contaminated. In response, communities, NGOs and state agencies began dedicated spring protection programmes. In the Himalayas, the State of Sikkim and organizations such as Central Himalayan Action and Research Group (CHIRAG) and People Science Institute (PSI) started identifying and protecting spring recharge areas around 2007. The difference between these programmes and many other previous efforts is that they went beyond supply-side improvements to focus on the use of hydrogeology to map springsheds for targeted interventions. The Advanced Centre for Water Resources Development and Management (ACWADAM), a research and capacity-building organization comprised of hydrogeologists and other experts began lending their expertise and building capacity of stakeholders. ACWADAM provides technical support, training and materials in hydrogeology to all network partners as well as others in India and the region. Similar programmes began independently in most of the mountain regions of India. Arghyam, a funding organization that was supporting many of these programmes, noticed that these disparate initiatives shared commonalities despite geographic diversity. They thus organized and funded a meeting of these various organizations in June 2014, and the Springs Initiative was born. The springs initiative aims to tackle the current water crisis and to ensure safe and sustainable access to water for all, by promoting responsible and appropriate management of aquifers, springsheds, and watersheds and conserving ecosystems in partnership with communities, governments and other stakeholders. This presentation has been developed as a part of the springs initiative to promote an understanding of springs and their role in mountainous areas.
Spring hydrogeology and its classification
Spring hydrogeology and its classification
India Water Portal
Lithological methods
Ground water exploration
Ground water exploration
HemanthKumar1131
An aquifer is an underground layer of water-bearing rock. Water-bearing rocks are permeable, meaning that they have openings that liquids and gases can pass through. Sedimentary rock such as sandstone, as well as sand and gravel, are examples of water-bearing rock.
Aquifer
Aquifer
Shah Naseer
Different types of Gw fluctuations are found in the earth. That's are controlling the factors of groundwater level
GROUNDWATER LEVEL FLUCTUATION
GROUNDWATER LEVEL FLUCTUATION
harikrishnankch
Groundwater province is an area or region in which geology and climate combine to produce groundwater conditions consistent enough to permit useful generalisations.
GROUNDWATER PROVINCES IN INDIA
GROUNDWATER PROVINCES IN INDIA
harikrishnankch
for my engineering pollution presentation
Saltwater intrusion
Saltwater intrusion
Muhammad Syahrizal
Contains materials related to hydrogeology
Hydrogeology
Hydrogeology
Pramoda Raj
Ground water
Ground water
Ground water
Shah Naseer
Groundwater
Groundwater
Groundwater
!SYOU co-designed sneakers
ARTIFICIAL RECHARGE OF GROUNDWATER
ARTIFICIAL RECHARGE OF GROUNDWATER
ARTIFICIAL RECHARGE OF GROUNDWATER
Namitha M R
DARCY’S LAW - hydroegeology
DARCY’S LAW
DARCY’S LAW
Pramoda Raj
salt water intrusion prevention & contgrol
Sea water intrusion
Sea water intrusion
Prashant Katti
All types of artificial recharge with explanation, figures etc.
Ground water recharge Methods
Ground water recharge Methods
Prabhat Mishra
Ground Water (Unit-V) Engg Geology
Ground Water (Unit-V)
Ground Water (Unit-V)
GAURAV. H .TANDON
1. Ground Water Occurrence 2. Types of Aquifers 3. Aquifer Parameters 4. Darcy’s Law 5. Measurement of Coefficient of Permeability of Soil 6. Types of Wells 7. Well Construction 8. Well Development
Groundwater Hydrology
Groundwater Hydrology
Malla Reddy University
Ground water is an essential and vital component of our life support system. therefore it is essential to check the ground water pollution.
GROUNDWATER QUALITY:- PROBLEMS CHALLENGES, & MANAGEMENT PROSPECTS IN INDIA
GROUNDWATER QUALITY:- PROBLEMS CHALLENGES, & MANAGEMENT PROSPECTS IN INDIA
Prashant Sharma
Vertical distribution of groundwater, types of groundwater, Rock properties affecting groundwater, Porosity, Soil classification, zone of saturation
Groundwater occurrence, Rock properties affecting groundwater, Soil classific...
Groundwater occurrence, Rock properties affecting groundwater, Soil classific...
Naresh Kumar
here are the 3 types of ground water
types of ground water
types of ground water
aki13
Type of Aquifer
Types of aquifer by bablu bishnoi
Types of aquifer by bablu bishnoi
VISHNU BARUPAL
Vertical distribution of groundwater
Vertical distribution of groundwater
Vertical distribution of groundwater
Pramoda Raj
groundwater
groundwater
Gladys Joy Bautista
review of land and soil degradation in India and Chhattisgarh
Land degradation and their restoration technology
Land degradation and their restoration technology
IGKV
IISTE Journals Call for paper: www.iiste.org/Journals
Topographic attributes control groundwater flow and groundwater
Topographic attributes control groundwater flow and groundwater
Alexander Decker
Contenu connexe
Tendances
Lithological methods
Ground water exploration
Ground water exploration
HemanthKumar1131
An aquifer is an underground layer of water-bearing rock. Water-bearing rocks are permeable, meaning that they have openings that liquids and gases can pass through. Sedimentary rock such as sandstone, as well as sand and gravel, are examples of water-bearing rock.
Aquifer
Aquifer
Shah Naseer
Different types of Gw fluctuations are found in the earth. That's are controlling the factors of groundwater level
GROUNDWATER LEVEL FLUCTUATION
GROUNDWATER LEVEL FLUCTUATION
harikrishnankch
Groundwater province is an area or region in which geology and climate combine to produce groundwater conditions consistent enough to permit useful generalisations.
GROUNDWATER PROVINCES IN INDIA
GROUNDWATER PROVINCES IN INDIA
harikrishnankch
for my engineering pollution presentation
Saltwater intrusion
Saltwater intrusion
Muhammad Syahrizal
Contains materials related to hydrogeology
Hydrogeology
Hydrogeology
Pramoda Raj
Ground water
Ground water
Ground water
Shah Naseer
Groundwater
Groundwater
Groundwater
!SYOU co-designed sneakers
ARTIFICIAL RECHARGE OF GROUNDWATER
ARTIFICIAL RECHARGE OF GROUNDWATER
ARTIFICIAL RECHARGE OF GROUNDWATER
Namitha M R
DARCY’S LAW - hydroegeology
DARCY’S LAW
DARCY’S LAW
Pramoda Raj
salt water intrusion prevention & contgrol
Sea water intrusion
Sea water intrusion
Prashant Katti
All types of artificial recharge with explanation, figures etc.
Ground water recharge Methods
Ground water recharge Methods
Prabhat Mishra
Ground Water (Unit-V) Engg Geology
Ground Water (Unit-V)
Ground Water (Unit-V)
GAURAV. H .TANDON
1. Ground Water Occurrence 2. Types of Aquifers 3. Aquifer Parameters 4. Darcy’s Law 5. Measurement of Coefficient of Permeability of Soil 6. Types of Wells 7. Well Construction 8. Well Development
Groundwater Hydrology
Groundwater Hydrology
Malla Reddy University
Ground water is an essential and vital component of our life support system. therefore it is essential to check the ground water pollution.
GROUNDWATER QUALITY:- PROBLEMS CHALLENGES, & MANAGEMENT PROSPECTS IN INDIA
GROUNDWATER QUALITY:- PROBLEMS CHALLENGES, & MANAGEMENT PROSPECTS IN INDIA
Prashant Sharma
Vertical distribution of groundwater, types of groundwater, Rock properties affecting groundwater, Porosity, Soil classification, zone of saturation
Groundwater occurrence, Rock properties affecting groundwater, Soil classific...
Groundwater occurrence, Rock properties affecting groundwater, Soil classific...
Naresh Kumar
here are the 3 types of ground water
types of ground water
types of ground water
aki13
Type of Aquifer
Types of aquifer by bablu bishnoi
Types of aquifer by bablu bishnoi
VISHNU BARUPAL
Vertical distribution of groundwater
Vertical distribution of groundwater
Vertical distribution of groundwater
Pramoda Raj
groundwater
groundwater
Gladys Joy Bautista
Tendances
(20)
Ground water exploration
Ground water exploration
Aquifer
Aquifer
GROUNDWATER LEVEL FLUCTUATION
GROUNDWATER LEVEL FLUCTUATION
GROUNDWATER PROVINCES IN INDIA
GROUNDWATER PROVINCES IN INDIA
Saltwater intrusion
Saltwater intrusion
Hydrogeology
Hydrogeology
Ground water
Ground water
Groundwater
Groundwater
ARTIFICIAL RECHARGE OF GROUNDWATER
ARTIFICIAL RECHARGE OF GROUNDWATER
DARCY’S LAW
DARCY’S LAW
Sea water intrusion
Sea water intrusion
Ground water recharge Methods
Ground water recharge Methods
Ground Water (Unit-V)
Ground Water (Unit-V)
Groundwater Hydrology
Groundwater Hydrology
GROUNDWATER QUALITY:- PROBLEMS CHALLENGES, & MANAGEMENT PROSPECTS IN INDIA
GROUNDWATER QUALITY:- PROBLEMS CHALLENGES, & MANAGEMENT PROSPECTS IN INDIA
Groundwater occurrence, Rock properties affecting groundwater, Soil classific...
Groundwater occurrence, Rock properties affecting groundwater, Soil classific...
types of ground water
types of ground water
Types of aquifer by bablu bishnoi
Types of aquifer by bablu bishnoi
Vertical distribution of groundwater
Vertical distribution of groundwater
groundwater
groundwater
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review of land and soil degradation in India and Chhattisgarh
Land degradation and their restoration technology
Land degradation and their restoration technology
IGKV
IISTE Journals Call for paper: www.iiste.org/Journals
Topographic attributes control groundwater flow and groundwater
Topographic attributes control groundwater flow and groundwater
Alexander Decker
Soil erosion is the removal and subsequent loss of soil by the action of water, ice, wind and gravity. Soil erosion is a process that occurs naturally at a slow rate. The average natural geologic rate of soil erosion is approximately 0.2 tons per acre per year. Erosion is the process were by the earth or rock is loosened or dissolved and removed from any part of earth‟s surface. Geological erosion is the rate at which the catchment or land would normally be eroded without any disturbance by human activity. If man alters the natural system by means of various land use practices that is caused accelerated erosion. The present study area is covering Parts of North Arcot The area is lies between E78°30'-E78°45' lattitudes N12°15'-N12°30„. The total aerial extent of the study area is 720 sq.km. It falls in the survey of India Toposheet 58 L11 on 1:50,000 scale. The IRS – 1D satellite imagery data were subjected to different types of image enhancement techniques and soil erosion areas were mapped out and GIS databases were generated showing the soil erosion areas using Arc Map 9.1 version. GIS overlay function was executed between soil erosion prone areas and the various controlling variables and the area has been fragmented into a number of polygons of land segments depending upon the controlling variables. Finally, the remedial measures were suggested for each land segment according to the controlling variables.
Identification Of Soil Erosion Prone Zones Using Geomatics Technology In Part...
Identification Of Soil Erosion Prone Zones Using Geomatics Technology In Part...
IJERA Editor
The integration of space born and ground remotely sensed data in exploring the environmental stresses and deterioration in ras gharib area, gulf of suez, egypt
The integration of space born and ground remotely sensed data
The integration of space born and ground remotely sensed data
oilandgas24
https://www.irjet.net/archives/V6/i5/IRJET-V6I5428.pdf
IRJET- Geotechnical Evaluation of Soils Found in Konso Town
IRJET- Geotechnical Evaluation of Soils Found in Konso Town
IRJET Journal
ABSTRACT: Advocated organic matter (OM) supplying to agriculture soil should be according to the soil properties, resulting different rates requirement instead of applying blank recommendation (12 tha-1 ). Two lowlands under continuous rice-rice cropping in the centre of Côte d’Ivoire were surveyed in 2013 considering 31 rice fields (farmers) for each location. Soil samples (93) were taken in 0 – 20 cm depth systematically (50 m along × 20 m across) extending the hydromorphic zone (HZ), the fringe valley (FV) and the valley bottom (VB) along the upper stream (US), median (MS) and downstream (DS) positions respectively. Soil organic carbon (SOC) content was differently observed in association with clay or silt particles according the topographic positions. Lowest amounts of SOC, maximum stable C (31.02% – 31.66%) and highest C mineralization (2.72% – 2.97%) rate (K2) were often accounting for the HZ contrasting with the VB. Unexpected higher rates of 224 tha-1 , 269.4 tha-1 and 281.03 tha-1 as rice and weed residues were required across the transversal section of the valley respectively over the current recommendation of 12 tha-1 . Dissolved C and leached nutrients (Na, K, Mg and Ca) may be released from HZ to VB contributing to rice yield gap (4.5 – 6.44 th-1 ). Soil contents of clay and K were the most relevant yield increasing factors against the contents of sand, silt and K2 value. More enriched organic-C source was required for improving organic input in the studied agro-systems emphasizing a major constraint for lowland rice production.
Soil Organic Carbon as observed in lowlands of Continuous Rice Cropping in Gu...
Soil Organic Carbon as observed in lowlands of Continuous Rice Cropping in Gu...
QUESTJOURNAL
The silt fractions have a great impact in soil structural formation. If the soil-forming rocks do not disturb, crush, and weather, the soil-forming processes on them occur weakly, the organic substances cause the formation of the loamy stratums without completely turning. This mostly influences the initial soil-forming layers. The reproduction minerals in these soils cause initial minerals majority by occurring weakly. If these processes occur quickly, then they cause a gradual increase of the reproduction minerals and reduction of the initial minerals. The heights of the zones where the geographical spreading of such stratums is situated depend on levels.
Impact of Mineral Formation on Restoration of the Soil Structure in Nakhchiva...
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BRNSS Publication Hub
8.isca rjrs-2012-188 done
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Mani Maran
The properties and potentials of soils of Liman Katagum (LK) in Bauchi State were assessed for both rainfed and irrigated crop production. Six soil mapping units were identified. The soils were moderately deep to very deep (93 – 163cm), except for exposed petroplinthite in some part of land unit LK 2. Soil pH ranged between 4.7 and 8.4, and was rated moderately acid to moderately alkaline. The soils were characterized by moderate fertility status. Improved management techniques were suggested for sustainable use of the land to improve farmers’ economy in the area. Assessment of the land potential showed that land units LK 3, LK 5 and LK6 (47.5%; 9.975ha) were moderately suitable (S2) and LK 1 and LK 4 (27.5%; 5.775ha) marginally suitable (S3) for rainfed crop production. For irrigated crop production, land units; LK 3, LK 4, LK 5 and LK 6 (51.43%; 10.8ha) were potentially moderately suitable (S2) and Land unit LK 1 (23.57%; 4.95ha) marginally suitable (S3). Land unit LK 2 constituting 25% (5.25ha) of the land was not potentially suitable (N2) for either rainfed or irrigated agriculture.
Properties and Potentials of Soils of Liman Katagum Bauchi State, Nigeria
Properties and Potentials of Soils of Liman Katagum Bauchi State, Nigeria
International Journal of Science and Research (IJSR)
The International Journal of Engineering and Science (The IJES)
The International Journal of Engineering and Science (The IJES)
theijes
FELIX PROJECT
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City of Hillasuffers from the high shallow groundwater levels which causes serious problems to agricultural and civil construction activities. five different tracks perpendicular to Shatt Al-Hilla channel are selected beside large number of hand dug wells within the area to monitor the relationships among the levels of water between these two water resources during one year,the results of many hydrochemical parameters confirm the similar pattern of inter-relationships between the two water bodies. According to hydrogeochemical measurements ,we find that the proportion of sulfates rate for these wells high and it hurts in the use of water for several purposes ,the ratio of chlorides and other high and this shows that the water wells unfit for uses of Agriculture purposes, but there is one well we have that shows the proportion of chlorides is a few , a high proportion of sulfates From Sholler classification of study area with high concentration of Na +k and SO4was observed because of the Fat'ha Formation, which contains gypsum, anhydrite and dolomite , are believed to be the major source of SO4 and Mg in the water
The Quality of Ground Water for Selected Area in South of Babylon Governorate...
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iosrjce
The paper is focused on the present state of soil protection from unwanted influences degradation through a process of water erosion. Agricultural land and forest land are a major component of the environment and it is therefore important to find tools for their protection. The paper presents empirical model used to determine the intensity of water erosion. We also will be presented options GIS tools in identifying areas threats with water erosion.
Methodology of Assessment Vulnerability of Soil Cover in Slovakia
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IJRES Journal
The 5th NENA Soil Partnership meeting 01 Apr 2019 - 02 Apr 2019 Cairo, Egypt Bahram Taheri
Implementation of the VGSSM in the Islamic Republic of Iran
Implementation of the VGSSM in the Islamic Republic of Iran
ExternalEvents
Geo-information and remote sensing are proper tools to enhance functional strategies for increasing awareness on natural hazard prevention and for supporting research and operational activities devoted to disaster reduction.
Gi4DM2010 GIS and geomatics for disaster relief
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Massimo Lanfranco
This presentation exhibit how to affect tsunami in soil properties. worldwide review.
C:\fakepath\Impact of tsunami on soil properties
C:\fakepath\Impact of tsunami on soil properties
sekaran
This paper presents an study Soil Properties analysis for sustainable agriculture by GIS through 15 soil samples chemical characterization conducts to soil numerical classification and crops soil suitability that has the advantage to guide the practices of soil management is as follows: Soil Salinity: The results of electrical conductivity indicated that the studied soils were generally positioned into the very saline class that had an area of (3847.96 ha) representing (79.50 %). The soils assembled into five classes; non-saline (198.5 ha) and it is suitable for most crops, moderately saline (385.75ha), where crops salt-tolerant crops give yield with marginal reduction. Finally, strong saline (112.00 ha) that it is suitable just for high salt-tolerant crops but also with yield reduction. Soil Sodic: the non-sodic soil class occupied the majority of the studied area with 96.8 % (4689.18 ha). The sodic soil had only (151.27 ha) 13.12 %. calcium carbonate to moderately calcareous soil (2317.93 ha) 47.89% and calcareous soil (2522.51 ha)52.11%. Crops soil suitability (Wheat): (S1), (S2) and (NS2) It is as follows (4000.78ha) 82.65 %, 114.37ha 2.36 %, and 725.30ha 14.98% of the studied area, respectively. (Tomato): is as follows: (4190.85 ha) 86.58 % of the study area is highly suitable (S1) and (NS2) (649.61ha) 13.42 % is unsuitable represent respectively. (Olive): The majority of the study area 4081.04 ha (84.31 %) was classified as highly suitable soils (S1), potentially suitable class (NS1) is about 236.61ha (4.89 %) and unsuitable class (NS2) is about (522.81ha) 10.80 % respectively. Soil Management and Crops tolerance for soil parameters The GIS-ESP soil map divided the studied area into three categories of ESP tolerance crops soil; Extremely sensitive ESP crop (4164.65 ha), sensitive ESP crop (594.13 ha) and moderately tolerant crop (81.67 ha). The GIS-CaCO3 soil map divided the studied area into two categories of CaCO3 tolerance crops soil; Crops that tolerate a certain (1924.92 ha) and Crops which support high (2915.54 ha). EC tolerance crops soil; Sensitive (3835.38 ha), moderately (224.28ha), highly (650.86 ha) and very highly (129.93ha).
GIS-Based Soil Properties Analysis for Sustainable Agriculture in Bani Waleed...
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2017 SWCS Annual Conference July 30-August 2, 2017 Monona Terrace Convention Center
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Ch2 occurrence-of-groundwater-1
1.
Environmental Engineering Department Water
Resources Management )3352EENV( Ch2: Occurrence of Groundwater -1 Instructor: Dr. Yunes Mogheir
2.
2. Occurrence of
Groundwater Rock Properties Affecting Groundwater Vertical Distribution of Groundwater Zone of Aeration Zone of Saturation Geological Formation as Aquifers -2 Geological Formation as Aquifers Types of Aquifers Storage Coefficient
3.
Rock Properties Affecting
Groundwater -3
4.
Porosity -4
5.
Porosity -5
6.
Porosity -6
7.
-7
8.
Soil Classification -8
9.
Soil Classification -9
10.
Soil Classification -10
11.
-11
12.
-12
13.
Vertical Distribution of
Groundwater -13
14.
Vertical Distribution of
Groundwater -14
15.
Zone of Aeration water
zone-. Soil1 -15
16.
Zone of Aeration zoneVadosIntermediate.2 -16
17.
Capillary zone.3 -17
18.
. Capillary zone3 -18
19.
SaturationZone of . Specific
Retention1 -19
20.
Yeild. Specific2 -20
21.
. Specific Yield2 -21
22.
Geological Formation as
Aquifers -22
23.
-23
24.
Types of Aquifers -24
25.
Types of Aquifers -25
26.
Types of Aquifers -26
27.
Storage Coefficient -27
28.
Storage Coefficient -28
29.
Gaza Aquifer Geological cross
section number 94 -29 Geological cross section number 95
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