This document discusses the importance of groundwater regime monitoring for groundwater management. It defines groundwater regime monitoring as collecting water level measurements from observation wells at regular time intervals to provide quantitative and qualitative information about groundwater. The key points are:
1) Groundwater monitoring is required to understand changes in groundwater quantity and quality over time due to slow hydrologic processes, and to design effective groundwater management programs.
2) A monitoring network is established with representative wells measured for water levels and quality quarterly.
3) Water level and quality data are analyzed statistically and spatially to identify trends and relationships helping groundwater management.
4) Challenges include data loss, high costs, and difficulty
Sea Water Intrusion(SWI) in coastal areas :
1. Occurrence of seawater intrusion
2.Factors that affect coastal aquifer
3.Changes by hydrological regime
4.Problems due to SWI
5.Ghyben-Herzberg relation
6.Methods to detect SWI
7.Control measures
Sea Water Intrusion(SWI) in coastal areas :
1. Occurrence of seawater intrusion
2.Factors that affect coastal aquifer
3.Changes by hydrological regime
4.Problems due to SWI
5.Ghyben-Herzberg relation
6.Methods to detect SWI
7.Control measures
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.
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
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.
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
Water is an important natural resource, which forms the cause of all life. Water is
one of the most requisite materials in our day to day life. It is a key resource in all
economic activities ranging from agriculture to industries. Only a minimal fraction of
the planet’s plentiful water is available to the living beings as fresh water. About 97%
is found in the oceans and is very salty for drinking, irrigation, or industry. The
remaining 3% is fresh water. About 2.997% of it is arrested in ice caps or glaciers or
is concealed so deep that it costs too much time & money to extract. Only about
0.0035 of Earth’s total volume of water is easily available to us as soil moisture,
exploitable ground water, water vapor, rivers, lakes and streams. In this present study
by a systematic sampling has been carried out to find the water quality parameters of
the Lake, by collecting samples from Six different positions, which covering entire
area of the lake, and the stations were distributed covering the periphery of the entire
tank, and also considering the inflow and the discharges and to suggest required
management techniques to make water free from the pollution
Surface water monitoring that how we do and what are the most objectives, methodology and scope that are in this ppt and it is very important for monitor a surface water that are shown in it
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1. SBL GSS Division
Groundwater Regime Monitoring and its
Significance in Groundwater Management
By
Venugopalan Nair
2. 2
Outline
1. Outline
2. Introduction
3. Why Groundwater monitoring is required
4. Groundwater Regime monitoring
5. Groundwater monitoring cycle
6. Period of measurement
7. Establishment of network stations
8. Base line data collection
9. Groundwater level data collection
10. Analysis of water level data
11. Groundwater scenario of India
12. Groundwater quality monitoring
13. Challenges in monitoring
14. Groundwater management through monitoring
3. 3
Self Introduction
Name: Venugopalan Nair
Education:
M.Sc. (Applied Geology), Barkatullah University, Bhopal, India
M.Tech (Remote Sensing), Bharathidasan University, Trichy, India
M.Tech (Hydrology), IIT, Roorkee, India
Experience: 15 Years + in GIS
National Geophysical Research Institute
GB Pant Institute of Himalayan Environment and Development
Defense Terrain Research Lab
Central Groundwater Board
RMSI
SBL
4. 4
Why Groundwater Regime Monitoring
Ground Water is extensive, concealed and inaccessible resource and its changes in
quantity and quality are through slow process.
Quick monitoring is not possible
Require long term monitoring and its analysis and interpretation
Is an indicative of hydrologic stresses undergone by aquifer which is having impacts on
Groundwater recharge, storage and discharge
Will help in design, implement and monitor the effectiveness of Groundwater
management, protection and conservation program.
Intervals depends on purpose
5. 5
Groundwater Regime Monitoring
Definition: Water level measurements from a network of
observation wells.
It is a collection of data, generally at set locations and depths
and a at regular time intervals in order to provide information
which may be used to determine the state of groundwater
both in quantitative and qualitative sense, provide the basis
for detecting trends in space and time, and enable the
establishment of cause-effect relationships.
Objective: Is to record information on Groundwater level and
quality through representative sampling in space and time
Time period: January, April/May, August, November (samples
on April/May)
Process involved:
Establishment of monitoring stations
Base line data collection
Data collection
Data storage and arrangements
Statistical and spatial analysis
Interpretation
6. 6
Period of Measurement
January - 1st to 10th of the month- represents the recession stage of water level
AprilMay - 20th to 30th of the month - represents water level of Pre-monsoon period
August - 20th to 30th of the month - represents peak monsoon water level
November - 1st to 10th of the month- represents water level of Post-monsoon period
8. 8
Establishment of network stations
A groundwater monitoring network is a system of dedicated Groundwater monitoring wells
in a geo hydrological unit at which Groundwater levels and water quality are measured at
pre-determined frequency.
Criteria:
It should be representative for hydro geological set up
There should be optimum number of stations based on management criteria
There should not be any immediate abstraction or drawdown effect
Station should be accessible
Station should be permanent and is representative of local area
There should be replacement possibilities
Due consideration of hydrological process in the unit
Monitoring stations can be
A key hole to aquifer
An abstraction well (tube well, bore well, or dug well)
Observation well
Piezometers
9. 9
Baseline data collection
Done at the time of development of a well
A static water level will be recorded as m bgl
Estimate altitude of the location with respect to mean
sea level in a msl
A well log will also be prepared
Water samples will be collected for individual aquifers
These analysis results will be recorded and retained for
further comparison
12. 12
Groundwater Level Scenario of India
Total number of NHNS: 12225
North of Ganges 2-5m bgl
North Western India 10-40m bgl
Delhi, parts of Rajasthan >40m bgl
East and West <10m bgl
Central India 2-5m bgl
Rice/Fall <2m 2-4m >4m
Rise in water level 46% 11% 5%
Fall in water level 28% 5% 2%
13. 13
Water Quality Monitoring
pH
TDS
EC
Total alkalinity
Ca, Mg, Na, K
Carbonate, sulphate, Fluoride, bicarbonate, nitrate, Chloride
Total anions, total cations
Sodium absorption ratio
Categorization of water into drinking, agricultural, industrial
etc
14. 14
Challenges in Groundwater Monitoring
Data loss during and after measurement
Inefficient use of man power and machinery
Expensive instruments and logistics
No visible return of investment
Difficulty in vertical variation in quantity and quality
Accuracy of the data
Monitoring of deeper and confined aquifers is difficult
15. 15
Groundwater Management Through Monitoring
Monitor impacts of abstraction on Groundwater system on a regional and local
scale
Groundwater balancing and budgeting
Calibration of numeric aquifer models
Determining pump usage and horse power
Determining the usage of water (potable, irrigable, industrial etc)
Early warning of potential threats in quantity and quality of Groundwater
Monitoring and managing of salt water intrusions
Monitoring of health hazards
To establish legal liabilities for pollution incidents and quantity issues
Monitoring droughts and floods
Monitoring water logging