Groundwater development for portable water supply
Table Of Contents
- <p> </p><p>Title page<br>Letter of transmittal<br>Dedication<br>Acknowledgement<br>Abstract<br>Table of contents<br>Introduction</p><p><b>
Chapter ONE
INTRODUCTION
- </b><br><b>
- 1.0 Historical background and groundwater theories</b><br>
- 1.1 Water theories<br>
- 1.2 Recent centuries</p><p><b>
Chapter TWO
LITERATURE REVIEW
- </b><br><b>
- 2.0 Importance of groundwater</b><br>
- 2.1 Groundwater in the hydrologic cycle<br>
- 2.2 Occurrence of groundwater<br>
- 2.3 Rock properties affecting groundwater<br>
- 2.4 Vertical distribution of groundwater<br>
- 2.5 Types of aquifers</p><p><b>
Chapter THREE
SYSTEM DESIGN AND IMPLEMENTATION
- </b><br><b>
- 3.0 Searching/exploration of groundwater</b><br>
- 3.1 Methods of groundwater exploration<br>
- 3.2 Groundwater basin investigation<br>
- 3.3 Data collection and fieldwork<br><b><br>
Chapter FOUR
SYSTEM TESTING AND EVALUATION
- <br>
- 4.0 Drilling for groundwater (wells)</b><br>
- 4.1 Test whole and well logs<br>
- 4.2 Methods for drilling shallow wells<br>
- 4.3 Methods for drilling deep wells<br>
- 4.4 Quality of groundwater<br>
- 4.5 Measures of water quality<br>
- 4.6 Water quality coterie</p><p><b>
Chapter FIVE
SUMMARY, CONCLUSION AND RECOMMENDATIONS
- <br>
- 5.0 Completion of wells</b><br>
- 5.1 Well development<br>
- 5.2 Protection of wells<br>
- 5.3 Well rehabilitation<br><b>
- 5.4 References</b></p> <br><p></p>
Project Abstract
<p> Groundwater hydrology may be defined as the science of the occurrence distribution, and movement of water below the surface of the earth. Geochydrology has an identical connotation, and hydrogeology differs only by its greater emphasis on geology. Utilization of groundwater dates from ancient times, although an understanding of the occurrence and movement of subsurface water as part of the hydrologic cycle has come only relatively recently.<br>SCOPE Groundwater referred to without specification is commonly understood to mean water occupying all the voids within geologic stratum. This saturated zone should be distinguished from an unsaturated, or earation zone where voids are filled with water and air. Water contained in saturated zone is important for engineering work, geologic studies and water supply development consequently, the occurrence of water in this zones will be emphasized here. Unsaturated zone a re usually found above saturated zones and extend uquad to the ground surface. Because this water includes soil masture within the root zone, it is a major concern for agriculture, binary, and soil science. No rigid demarcation of water between the two zones is possible, for they possess an interdependent boundary and water can move from owe zone to the other in either direction. The interrelationships are described more in some higher hydrogeology texts. <br></p>Project Overview
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