Wednesday, 4 February 2015

Development of engineering geology

INTRODUCTION: While ancient man must have had some intuitive knowledge of geology, as evidenced by the feats of mining and civil engineering performed in the distant past, the present science of geology owes much of its origin to the civil engineers working in the eighteenth century. These engineers, while constructing the major engineering works associated with the industrial revolution, had the opportunity to view and explore excavations in rocks and soils. Some, intrigued by what they saw, began to speculate on the origin and nature of rocks, and the relationships between similar rocks found in different places. Their ideas and theories, based on the practical application of their subject, formed the groundwork for the development of geology as a science. Engineers such as Lewis Evans (1700–1756) in America, William Smith (1769–1839) in England, Pierre Cordier (1777–1862) in France and many others were the ‘fathers’ of Geology.

Their interest in geology often stemmed from a ‘need to know’. They were confronted with real engineering problems which could only be solved with the help of both knowledge and understanding of the ground conditions with which they were confronted. In the later nineteenth century both geology and engineering advanced, geology becoming a more-or-less respectable natural philosophy forming part of the education considered suitable for well brought up young ladies. Engineering, characterized by the canal and railway construction carried out by the ‘navvy’, on the other hand, remained as an eminently practical subject. The theoretical understanding of engineering was driven by practical engineering problems. The geological knowledge of the engineer, confronted by increasingly difficult engineering challenges, did not progress as rapidly as geology, advanced as a science under the leadership of geologists such as James Dana (1813–1895) in America, Albert Heim (1849–1937) in Switzerland and Sir Archibald Geikie (1835–1924) in Britain. Thus, by the end of the nineteenth century the majority of civil engineers knew relatively little about geology, and very few geologists were concerned about, or interested in, its engineering applications.

This widening division between geology and engineering was partly bridged in the nineteenth and early twentieth century by the development of soil mechanics by engineers such as Charles Coulomb and Macquorn  Rankine, who developed methods of calculating the deformations of earth masses under the stresses imposed by engineering works. The great leap forward may be considered to have taken place with the publication of “Erdbaumechanik” by Karl Terzaghi in 1925, which brought together old knowledge, and added new theory and experience to establish soil mechanics in its own right as a discipline within the field of civil engineering. Subsequent publications by Terzaghi and others have continued to recognize a clear understanding of the fundamental importance of geological conditions in civil engineering design and construction. However, this appreciation has not proved to be universal and many engineers continued to rely on inadequate geological knowledge, or over-simplified ground models.

Aims of Engineering Geology: Every discipline must have an aim and purpose. The Association of Engineering Geologistsincludes in its 2000 Annual Report and Directory the following statement:“Engineering Geology is defined by the Association of Engineering Geologists as the disciplineof applying geologic data, techniques, and principles to the study both of a) naturally occurringrock and soil materials, and surface and sub-surface fluids and b) the interaction of introducedmaterials and processes with the geologic environment, so that geologic factors affecting the planning,design, construction, operation and maintenance of engineering structures (fixed works)and the development, protection and remediation of ground-water resources are adequatelyrecognized, interpreted and presented for use in engineering and related practice.”The IAEG has produced a statement on similar lines which sets out the redefinitionof its mission in 1998 as The International Association for Engineering Geologyand the Environment.The exact phraseology, and interpretation, of such statements varies from countryto country depending upon national and local practice. Thus many “engineering geologists”are essentially geologists who deliver basic geological data to engineers, withoutinterpretation. At the other end of the scale some engineering geologists mightdesign foundations and slope stabilization, thereby spending much of their time asgeotechnical engineers. Much clearly depends on the training and experience of thegeologist involved, and the attitudes of the organization in which he or she is employed.A particular problem lies in the field of hydrogeology (or geohydrology). In somecountries much of exploration for sources of potable water is carried out by engineeringgeologists. In other countries this is undertaken by specialized hydro geologists whoare quite separate from their engineering geological brethren. Again the national culture of science and engineering influences the trend. Engineering geology may exist under, or be a part of, other titles, such as “geological engineering”, “geotechnical engineering”, “earth science engineering”, “environmental geology”, “and engineering geomorphology” and so on. If there is a difference in the content of the disciplines described under these names it probably lies in the training and experience of the practitioner. Engineering geology is taught in some countries as a postgraduate (Masters) degree course following on from a first degree or other qualification. If the first degree is in geology then the product after the Master’s degree will be that of an engineering geologist; if the first degree is in engineering then the product may be considered as a geotechnical engineer.

Geological Sciences

What is Geological Sciences: 

Geology is the study of the Earth, its composition, its history, and its constantly changing character. Geologists study the origin and evolution of our planet; the chemical and physical properties of minerals, rocks, and fluids; the structure of our mobile crust - it’s newly forming ocean floors and its ancient drifting continents; the history of life; and the human adaptation to earthquakes, volcanoes, landslides and floods. The subject matter of geology ranges from dinosaurs to the prediction of earthquakes. If you are intensely curious about the planet on which we live, challenged by problems which involve the Earth, and are intrigued by the potential of a subject which combines the best of both the arts and sciences, geology is a major you should consider. Geology attracts women and men who love the outdoors and thrive on practical challenges. In addition to a basic field component, the earth sciences employ much of the sophistication of chemistry, physics and engineering to interpret the nature, origin and usefulness of minerals, rocks, soils, oceans, groundwater and atmosphere.

Why is Geology important? Geology is the study of the Earth and how it works.  Geologists investigate processes that operate at and below the surface of the Earth, and the materials in which these processes occur.  Geologists not only look at the present-day processes, but they examine the historic record of geologic events preserved in the rock record. Believe it or not, geology is all around us - not just in the mountains or oceans, but we actually see geology and depend on geologic resources in our everyday lives.  For example, if you wanted to construct a building, you would need geologic materials for construction such as gypsum, limestone, clay, sand, gravels, to name a few. Globally, we face natural hazards of one sort or another.   Earthquakes, volcanic eruptions, floods, droughts, groundwater pollution, hurricanes... all are dynamic processes taking place even as you read this.  We can't prevent hazards from occurring.  But, if we study the past and present record of these events, we can gain a better idea of how these processes work and help predict and prepare for future events. And yes, geology does involve looking at rocks.  But there is so much information locked up in these rocks that can help us better predict the behavior of the Earth.   Geologists keep busy trying to find, develop, and conserve natural resources.   Geologists investigate our water supplies and strive to keep them clear of pollutants.  Geologists are working to determine the controls on, and lessen the effects of, natural hazards.

What do Geologists do?

Whether you are interested in fieldwork or in the laboratory, geology offers you many options for an interesting career. You might work with a rock hammer, a drilling rig, a microscope, a computer or with scale models such as wind tunnels. You might even reach the moon!

Geologists investigate the materials, processes, products and history of the Earth. They often specialize in one of the following areas:

Hydro geologists: study the abundance, distribution and quality of ground water.

Environmental geologists: work to solve problems with pollution, waste disposal and urban development and hazards such as flooding and erosion.

Geo morphologists: study the effects of Earth processes and investigate the nature, origin and development of present landforms and their relationship to underlying structures.

Pale climatologists/Pale oceanographers: interpret past global changes and predict future changes from past records.

Volcanologists: investigate volcanoes and volcanic phenomena.

Seismologists: study the location and force of earthquakes and trace the behavior of earthquake waves to interpret the structure of the Earth.

Petroleum geologists: are involved in exploration and production of oil and natural gas.

Economic geologists: explore for and develop geologic materials that have profitable uses.

Engineering geologists: investigate geologic factors that affect engineering structures such as bridges, buildings, airports and dams.

Geochemists: investigate the nature and distribution of chemical elements in rocks and minerals.

Pathologists: determine the origin and genesis of rocks by analyzing the textures and chemistry of minerals and rocks.

Earthquakes

Earthquakes:

An earthquake is a major demonstration of the power of the tectonic forces caused by endogenetic thermal conditions of the interior of the earth. An earthquake is a motion of the ground surface, ranging from a faint tremor to a wild motion capable of shaking buildings apart and causing gaping fissures to open in the ground. The Richter scale devised by Charles F. Richter in 1935 measures the magnitude or intensity of energy released by an earthquake. Good Friday Earthquake of March 27, 1964 in Alaska (USA) measuring 8.4 to 8.6 on Richter scale is among the greatest earthquakes of the world ever recorded.

Causes of Earthquakes:

Earthquakes are caused mainly due to disequilibria in any part of the crust of the earth. A number of causes have been assigned to cause disequilibria in the earth’s crust such as volcanic eruptions, faulting and folding, gaseous expansion and contraction inside the earth, hydrostatic pressure of man-made water bodies like reservoirs and lakes, and plate movements.

(1) Vulcan City:

Volcanic activity is considered to be one of the major causes of earthquakes. Vulcan city and seismic events are so intimately related to each other that they become cause and effect for each other. Earthquakes follow each volcanic eruption and many of the severe earthquakes cause volcanic eruptions. The explosive violent gases during the process of Vulcan city try to escape upward and hence they push the crystal surface from below with great force and thus is’ caused severe earth tremors of high magnitude.

(2) Faulting and Elastic Rebound Theory:

The horizontal and vertical movements caused by end genetic forces result in the formation of faults and folds which in turn cause isocratic disequilibria in the crystal rocks which ultimately causes earthquakes of varying magnitudes depending on the nature and magnitude of dislocation of rock blocks caused by faulting and folding. The 1950 earthquake of Assam was believed to have been caused due to disequilibria in crystal rocks.

(3) Hydrostatic Pressure and Anthropogenic Causes:

Certain human activities such as pumping of ground water and oil, deep underground mining, blasting of rocks by dynamites for constructional purposes, nuclear explosion, storage of huge volume of water in big reservoirs etc. also cause earth tremors of serious consequences. The introduction of additional load through the construction of large dams and impounding of enormous volume of water in big reservoirs behind the dams cause disequilibria of adjusted rocks below the reservoirs.

(4) Plate Tectonic Theory:

The earth is composed of solid and moving plates having either continental crust or oceanic crust or even both continental oceanic crusts. The earth’s crust consists of 6 major plates (Eurasian plate, American plate, African plate, Indian plate, Pacific plate and Antarctic plate) and 20 minor plates. These plates are constantly moving in relation to each other due to thermal convective currents originating deep within the earth. All sorts of disequilibria are caused due to different types of plate motions and consequently earthquakes of varying magnitudes are caused.

Effects of Earthquake hazardous: Earthquakes and their hazards are determined on the basis of the magnitude of seismic intensity as determined by Richter scale but are decided in the basis of quantum of damages done by a specific earthquake to human lives and property.

(i) Landslides:

Weaker landmasses and tectonically sensitive land margins cause landslides and debris falls, which damage settlements and transport systems on the lower slope segments.

(ii) Damage to Life and property:

Structures such as buildings, roads, rails, factories, dams, bridges suffer a huge damage thus causing a heavy loss of human life and property both. The vibrations of earthquakes last longer and the amplitudes of seismic waves are greater artificially in filled and leveled depressions, swamp deposits etc. than in the structures of consolidated materials and bedrocks. Two major earthquakes of Bihar-Nepal border in 1934 and 1988 explain the impact of earthquake disasters on human structures and human lives. The damage caused by the Bihar earthquake of 15 January 1934, measuring 8.4 on Richter scale, include 10,700 human deaths, landslides and slumping in an area of 250 km length and 60 km width, ruptures and faults in the ground surface etc.

(iii) Damages to Government Infrastructure:

Cities and towns are worst affected due to large concentration of human population, commercial complexes and residential areas. Due to collapse of large buildings there is greater loss of life and property. Due to collapse of buildings ground water pipes are bent and damaged thus water supply is disrupted, electric and telephone poles are uprooted and there is total disruption of power and communication. Other side effects are collapsed sewer system causing epidemics, roadblocks etc.

(iv) Fire Hazard:

Earthquakes strongly shake the buildings and thus strong oscillations cause severe fires in houses, mines and factories because of overturning of cooking gas cylinders, contact of live electric wires, churning of blast furnaces, displacement of other electric and fire related appliances.

(v) Landmass Deformation:

Severe earth tremors and resultant, vibrations caused by severe earthquakes result in the deformation of ground surface because of crusts and troughs in the ground surface and faulting activity.

(vi) Tsunamis:

The seismic waves, caused by the earthquakes traveling through seawater, generate high sea waves and cause great loss of life and property. Since the Pacific Ocean is girdled by the earthquakes and volcanoes tsunamis are more common in the pacific with a minimum frequency of 2 tsunamis per year.

Monday, 2 February 2015

Branches of GEOLOGY

  • Economic geology
  • Mining geology
  • Petroleum geology
  • Engineering geology
  • Environmental geology
  • Geochemistry
  • Geological modelling
  • Geomorphology
  • Geophysics
  • Historical geology
  • Hydrogeology
  • Mineralogy
  • Paleontology
  • Petrology
  • Sedimentology
  • Stratigraphy
  • Structural geology
  • Volcanology




Economic geology:

Economic geology is concerned with earth materials that can be used for economic and/or industrial purposes. These materials include precious and base metals, nonmetallic minerals, construction-grade stone, petroleum minerals, coal, and water. The term commonly refers to metallic mineral deposits and mineral resources. The techniques employed by other earth science disciplines (such as geochemistrymineralogygeophysicspetrology and structural geology) might all be used to understand, describe, and exploit an ore deposit.
Economic geology is studied and practiced by geologists. However it is of prime interest to investment bankers, stock analysts and other professions such as engineers, environmental scientists, and conservationists because of the far-reaching impact that extractive industries have on society, the economy, and the environment.

Mining Geology:

Mining is the extraction of valuable minerals or other geological materials from the earth from an orebodylodeveinseam, or reef, which forms the mineralized package of economic interest to the miner.
Ores recovered by mining include metalscoaloil shalegemstoneslimestonedimension stonerock saltpotashgravel, and clay. Mining is required to obtain any material that cannot be grown through agricultural processes, or created artificially in a laboratory orfactory. Mining in a wider sense includes extraction of any non-renewable resource such as petroleumnatural gas, or even water.
Mining of stone and metal has been done since pre-historic times. Modern mining processes involve prospecting for ore bodies, analysis of the profit potential of a proposed mine, extraction of the desired materials, and final reclamation of the land after the mine is closed.
The nature of mining processes creates a potential negative impact on the environment both during the mining operations and for years after the mine is closed. This impact has led most of the world's nations to adopt regulations designed to moderate the negative effects of mining operations. Safety has long been a concern as well, and modern practices have improved safety in mines significantly.

Petroleum geology:

Petroleum geology is the study of origin, occurrence, movement, accumulation, and exploration of hydrocarbon fuels. It refers to the specific set of geological disciplines that are applied to the search for hydrocarbons (oil exploration).

Engineering geology

Engineering geology is the application of the geologic sciences to engineering study for the right of assuring that the geologic factors regarding the location, design, construction, operation and maintenance of engineering works are recognized and made for Engineering geologists investigate and provide geologic and geotechnical recommendations, analysis, and design associated with human development. The realm of the engineering geologist is essentially in the area of earth-structure interactions, or investigation of how the earth or earth processes impact human made structures and human activities.
Engineering geologic studies may be performed during the planning, environmental impact analysis, civil or structural engineering design, value engineering and construction phases of public and private works projects, and during post-construction and forensic phases of projects. Works completed by engineering geologists include; geologic hazards,geotechnical, material properties, landslide and slope stability, erosionfloodingdewatering, and seismic investigations, etc. Engineering geologic studies are performed by ageologist or engineering geologist that is educated, trained and has obtained experience related to the recognition and interpretation of natural processes, the understanding of how these processes impact man-made structures (and vice versa), and knowledge of methods by which to mitigate for hazards resulting from adverse natural or man-made conditions. The principal objective of the engineering geologist is the protection of life and property against damage caused by geologic conditions.
Engineering geologic practice is also closely related to the practice of geological engineeringgeotechnical engineeringsoils engineeringenvironmental geology and economic geology. If there is a difference in the content of the disciplines described, it mainly lies in the training or experience of the practitioner.

Environmental geology

Environmental geology, like hydrogeology, is an applied science concerned with the practical application of the principles of geology in the solving of environmental problems. It is a multidisciplinary field that is closely related to engineering geology and, to a lesser extent, to environmental geography. Each of these fields involves the study of the interaction of humans with the geologic environment, including the biosphere, the lithosphere, the hydrosphere, and to some extent the atmosphere.In other words Environmental geology is the application of geological information to solve conflicts, minimizing possible adverse environmental degradation or maximizing possible advantageous condition resulting from the use of natural and modified environment.
Environmental geology includes:
  • managing geological and hydrogeological resources such as fossil fuelsmineralswater (surface and ground water), and land use.
  • studying the earth's surface through the disciplines of geomorphology, and edaphology;
  • defining and mitigating exposure of natural hazards on humans
  • managing industrial and domestic waste disposal and minimizing or eliminating effects of pollution, and
  • performing associated activities, often involving litigation.

What Does a Geologist Do?


 

Geologists work to understand the history of our planet. The better they can understand Earth’s history the better they can foresee how events and processes of the past might influence the future. Here are some examples: 

Geologists study earth processes:   Many processes such aslandslidesearthquakesfloods and volcanic eruptions can be hazardous to people. Geologists work to understand these processes well enough to avoid building important structures where they might be damaged. If geologists can prepare maps of areas that have flooded in the past they can prepare maps of areas that might be flooded in the future. These maps can be used to guide the development of communities and determine where flood protection or flood insurance is needed. 

Geologists study earth materials:   People use earth materials every day. They use oil that is produced from wells, metals that are produced from mines, and water that has been drawn from streams or from underground. Geologists conduct studies that locate rocks that contain important metals, plan the mines that produce them and the methods used to remove the metals from the rocks. They do similar work to locate and produce oil, natural gas and groundwater. 

Geologists study earth history:   Today we are concerned aboutclimate change. Many geologists are working to learn about the past climates of earth and how they have changed across time. Thishistorical geology news information is valuable to understand how our current climate is changing and what the results might be. 

What is geology?

Geology is the study of the Earth, its processes, its materials, its history, and its effect on humans and life in general.  Rocks, crystals, mountains, earthquakes, volcanoes, rivers, glaciers, landslides, floods, and many other subjects fall into this broad field of research.  Geologists perform a wide range of important services for our civilization: they determine the stability of building sites, find abundant supplies of clean water, search for valuable deposits of natural resources such as iron, coal, and oil, and they also try to minimize the threat to communities at risk from geologic hazards.

Geology is special in that it is a highly field-oriented science.  A geologist's work is usually outdoors, sometimes in out-of-the way places such as deserts or sparsely populated mountain ranges.  Some of the most geologically interesting places in the world are also the most scenic.  Students of geology can expect to find themselves working in locales that they have often wanted to travel to, as well as many that they had not known of but were grateful to have visited still.

Geology is a very visual science.  Many problems in geology are much like solving a puzzle.  A common task for students is to present a possible explanation of the events that occurred to produce the scenery surrounding them.  If you have ever wondered how a certain hill came to exist in a certain place, or why a cliff or canyon should have such a vivid display of color to it, or why a large outcrop of rock is exposed in a particular fashion, a background in geology can help you to return to those features and figure out the answers.  Once you have had an introduction to geology, you will see the world around you in a completely new light.