Notes, summaries, assignments, exams, and problems for Geology

Earth and Geographic Features

Circles perpendicular and parallel to the terrestrial axis are parallel. Ecuador, at 0 degrees, is a semicircle. Meridians go from pole to pole. Meridian 0 degrees passes through Greenwich.

Latitude and Longitude

Latitude is the angular distance from any point of land to Ecuador. Longitude represents the distance from meridian 0.

Maps and Relief

A map proportionally represents land or a part of it. Geography is the science that studies landscapes, understood as a set of physical and human elements that relate to each other.

Relief is the set of forms that the Earth's surface presents, shaped by terrestrial forces.

Morphostructural Units

Organic and erosive forms are the internal disposition that relief takes. Erosion is... Continue reading "Earth Science: Landforms, Climate, and Water Flow" »

Energy is the capacity of a body or system to make changes.

Forms of Energy

As per the law of conservation of energy, "Energy is neither created nor destroyed, only transformed." Energy can manifest itself in several ways:

• Mechanical energy: Associated with motion (e.g., lifting a backpack).
• Thermal energy: Related to temperature (e.g., warm water).
• Chemical energy: Associated with chemical reactions (e.g., coal combustion).
• Nuclear energy: Derived from the decay of radioactive substances.
• Radiant energy: Associated with electromagnetic radiation (e.g., light, microwaves).
• Electrical energy: Related to the movement of electric charges.

Energy Sources and Classifications

We refer to conventional sources as those that provide most of the energy in various... Continue reading "Energy Fundamentals: Forms, Sources, and Production" »

Conventional Electricity Generation Methods

Conventional energy sources are currently the most significant contributors to global power generation:

• Thermal Power Generation

  Thermal power plants burn fuel to produce heat, which converts water into high-pressure steam. This steam then moves turbines connected to electrical generators, producing electricity. Coal is the most commonly used fuel in these plants.

• Nuclear Power Generation

  Nuclear power is produced from the fission (or breaking apart) of atoms of radioactive minerals, primarily uranium. This fission process, carried out in nuclear power plants, generates heat that warms water to create high-pressure steam. The steam drives turbines, which in turn generate electricity.

• Hydropower Generation

  Hydropower

Ocean Thermal Energy Conversion (OTEC)

Closed-Loop Systems

In a closed-loop OTEC system, a working fluid with a low boiling point, such as ammonia, is heated by warm surface seawater. This causes the fluid to vaporize into steam, which then drives a turbogenerator to produce electricity. Cold deep-ocean water is used to condense the vapor back into a liquid, allowing the cycle to repeat.

Open-Loop Systems

Open-loop OTEC systems directly use warm surface seawater as the working fluid. The warm seawater is flash-evaporated in a vacuum chamber, creating low-pressure steam. This steam then drives a turbine. Cold deep-ocean water condenses the steam, producing desalinated fresh water as a byproduct.

Benefits of OTEC

• Renewable Energy Source: Utilizes the

Definitions

• Principle of Actualism: Analyzing present processes is key to interpreting past events.
• Relative Dating: Establishes the order of events without numerical ages.
• Absolute Dating: Provides numerical ages for events (e.g., years or millions of years ago).
• Stratification Planes: Surfaces that delimit layers (strata).
• Roof: The uppermost and youngest part of a stratum.
• Wall (Base): The lowermost and oldest part of a stratum.
• Series Roof: The top and youngest part of a series of strata.
• Series Wall: The bottom and oldest part of a series of strata.
• Thickness: The vertical distance between the roof and wall of a stratum.
• Polarity Criteria (Roof-Wall): Sedimentary structures that help determine the orientation of strata.
• Concordance: Two materials

Understanding Geological Processes

Weathering: Alteration of Rocks

Weathering is the alteration of rocks by atmospheric and biological agents in situ (in the same place where they are found). It differs based on the type of alteration:

• Chemical Weathering: This involves the chemical alteration of rocks resulting from reactions such as oxidation and dissolution.
• Mechanical Weathering: Also known as physical weathering, this is the physical alteration of rocks due to sudden changes in temperature, pressures caused by the freezing of water that fills cracks, or the growth of plant roots.

A specific example of chemical weathering is Carbonation Dissolution. This occurs when rainwater and atmospheric carbon dioxide (CO2) combine to form carbonic acid.... Continue reading "Geological Processes: Weathering, Sedimentation, and River Dynamics" »

The Book of Good Love: Text, Author, and Context

The Book of Good Love is attributed to Juan Ruiz, also known as the Archpriest of Hita. The work survives in three manuscript copies and several fragments. The author identifies himself as Juan Ruiz. Limited information exists about him.

Manuscript Dates and Versions

The manuscripts contain two dates, 1330 and 1343, suggesting that there were two successive versions of the book. This accounts for the differences between the texts. However, some scholars believe the work to be a single redaction, arguing that the variations among the manuscripts reflect the complexities of transmitting medieval texts. None of the manuscripts bear the title Book of Good Love; this title was assigned later.

Language,

Soil Evolution and Degradation

Soils evolve while newly forming soils are simultaneously destroyed due to erosion. There are two primary scenarios:

• Scenario 1: If predominant soil-forming processes lead to thicker soils, though not indefinitely. In the upper layers, plant debris accumulates, and decomposers are active. In the lower layers, bedrock breaks down, even at significant depths.
• Scenario 2: If soil erosion predominantly causes thickness loss, the parent rock may become exposed, initiating the soil formation process anew.

Human Impact on Soil Degradation

Soils are degraded and destroyed by various human activities that decrease their quality and fertility:

1. Deforestation or Forest Clearing: For timber or agriculture, which significantly facilitates

Tributary

River that flows into another, larger river.

Stream

A small, continuous flow of water in a channel.

Flash Flood

Sudden, violent increase in water level flowing down a stream or dry channel, occurring abruptly in areas with steep slopes.

Water Balance

The relationship between available water resources and their use. In Spain, this balance is currently considered positive.

Flow (Discharge)

The amount of water flowing through a river channel at a specific point in time, typically measured in cubic meters per second.

Instantaneous Flow

The instantaneous amount of water passing a specific point in a river per second.

Hydrographic Basin (Drainage Basin)

The territory where all surface water drains to a common point, such as a river, lake, or ocean.... Continue reading "Hydrology Terms Defined" »

Primary Treatment

Primary treatment aims to reduce oils, grease, sand, and thick solids using machinery.

Removal of Solids

During mechanical treatment, the effluent is filtered through chambers with bars to remove all large objects that are deposited in the sewer system. Biological treatments are not designed to deal with these solids.

Sand Stripping

This equipment is called a sand trap. Sand and stones need to be removed in time during the process to prevent damage to pumps and other equipment in the remaining phases of treatment.

Primary Sedimentation Tank in Rural Treatment Plants

Research and Maceration

Solids are cut into small particles through the use of rotating blades mounted on a revolving cylinder. This is utilized in plants that can process... Continue reading "Wastewater Treatment: Primary and Secondary Stages" »