WEEK 3 DISCUSSION ENV
docx
keyboard_arrow_up
School
University of Phoenix *
*We aren’t endorsed by this school
Course
400
Subject
Geology
Date
Jan 9, 2024
Type
docx
Pages
3
Uploaded by AmbassadorDinosaurPerson162
WEEK 3 DISCUSSION ENV/400
Hello class,
My research into the geological influences that are exerted on water began with an analysis into the mechanisms that are responsible for water penetrating soils.
I researched the processes of infiltration, percolation, and runoff, as well as the ways in which each process influenced the quantity of water that was accessible. Specifically, I looked at how each process affected the amount of water that was available. In addition, I researched the underlying geology of the region, which included determining the composition of the different layers of soil
and the degree to which the soils allowed water to pass through them. As part of
my study, I investigated the geological processes that control the storage and flow of water through groundwater networks. These geological mechanisms regulate the storage and circulation of water. In addition to this, I investigated how the consequences of climate change may become apparent in the form of differing degrees of accessibility to water in different parts of the nation. The culmination of all of these studies contributed to the development of a more profound grasp of the geological causes that influence water.
My comprehension of the intricacies of the processes that are involved in deciding the quantity of water that is accessible has improved as a result of the research that I conducted. I was able to get an awareness of how a variety of factors, such as the permeability of the soils, the level of the water table, and the climate, all play a role in determining the amount of water that is stored and
conveyed. I now have a greater understanding of the relevance of water resource management that is not only efficient but also ecologically responsible thanks to the new knowledge I have obtained.
Both my knowledge and my thoughts on this topic have been significantly impacted as a direct result of my study into the geological elements that govern
water. My research has provided me with the opportunity to get a more in-depth
grasp of the manner in which geological processes impact the accessibility of water. As a direct consequence of this experience, I now have a deeper comprehension of the intricate processes involved in the warehousing and transportation of water, which has significantly enriched my knowledge in this area.
In addition to this, I have gained a more profound understanding of the necessity of engaging in water management practices that are ecologically responsible. Because of my research, I am now aware that in order to successfully manage water resources, it is vital to take into account a lot of different variables at the same time. This is something that I was previously unaware of. As a result of gaining this knowledge, I now have a better respect for the need of water management systems that are both effective and sustainable.
Increasing my understanding of the several methods that may be used to determine whether or not an environmental problem exists would be of tremendous help to the job that I do in the field of environmental science. If I am
able to properly identify environmental issues and find solutions to those issues,
not only will I have an edge over other people working in my industry, but I will also be in a position to be of greater assistance to the community as a whole.
Not only would having an understanding of the several strategies at my disposal
for discovering environmental challenges help me provide solutions that are more effective, but it will also make room for my own personal development and
development of my skills. With this knowledge, I will be able to discover the core
problem that is producing a problem in the environment and construct remedies
that are especially geared to solve that problem. Moreover, I will be able to take action to remedy the problem. Because of this, I will be able to provide the community a greater degree of service and ensure that the solutions will be effective as well as long-lasting.
My grasp of the dynamics of hydrologic systems is intricately connected to the geological processes that I am familiar with. When trying to appreciate the path that water takes through the subsurface, for instance, it is vital to take into consideration the geology of the location. The geology of the area has an influence on the overall amount of water that is held below ground as well as the degree to which the various soil layers allow water to move through them. This is because the different soil layers have varied permeabilities. Furthermore,
the water table denotes the topmost limit of the underground water, and the depth to which the water table extends is determined by the geology of the area
that surrounds the water table.
In addition, the quantity of water that is easily available may be affected by a number of variables, including the permeability of the ground, the make-up of
the rock that lies under the surface, and the composition of the soil. Porosity is the ability of a material to hold water, and the kind of rock that is present in a location may have an influence on the permeability of the soil in that area. This information may be useful in determining the most appropriate locations for water wells and other types of water resources, such as rivers and lakes. Gaining a knowledge of the geology of the area may also help in the identification of potential sources of pollution, and it can serve as a foundation for the creation of measures that are intended to protect water resources.
The "water table" is a term that is used to denote the uppermost boundary of the subterranean water, as well as the limit that is referred to by that term. It is the level of water in the ground that is attainable for consumption and may be thought of as an underground reservoir. In common usage, it is referred to as "ground water." In the event that a well were to be excavated, but the water table was too low, it would be challenging to get the water that was contained inside the well.
The term "restricted" is the one that is used the most often when discussing the pressure that is present in groundwater systems. This is because of the nature of this pressure. The amount of pressure that is imposed on the groundwater is one way that common language may be used to speak about this occurrence. [Citation needed] [Citation needed] In the event that an aquifer is enclosed, for example, the pressure of the groundwater contained inside will be greater than the pressure of the air found outside. It is possible that the water may get encased in the subsoil as a result of this, which will prevent the water from flowing out of the aquifer. Additionally, due of the higher pressure, confined aquifers are more resistant to contamination than open ones. This is because of the greater water pressure. Because of the pressure, any impurities that could be present in the air are kept out of the water.
1. Tucci, P. (n.d.). Groundwater Hydrology: Infiltration, Percolation, and Runoff. https://www.gracelinks.org/blog/groundwater-hydrology-infiltration-percolation-
and-runoff
2. USGS. (n.d.). Water Table. https://water.usgs.gov/edu/watertable.html
3. USGS. (n.d.). Confined Aquifers. https://water.usgs.gov/edu/confined.html
Your preview ends here
Eager to read complete document? Join bartleby learn and gain access to the full version
- Access to all documents
- Unlimited textbook solutions
- 24/7 expert homework help