Evaporation: Hydrological Process
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Which of the following best describes the process of evaporation?

  • The change of a gas to a liquid state at the boiling point with a release of heat.
  • The change of a solid to a liquid state below the melting point through the release of energy.
  • The change of a liquid to a gaseous state at the free surface below the boiling point through the transfer of heat energy. (correct)
  • The change of a liquid to a gaseous state at the boiling point with an absorption of heat.

Why is evaporation considered a cooling process?

  • Because the water body gains heat from the surroundings.
  • Because the escaping water molecules have lower kinetic energy.
  • Because the latent heat of vaporization must be supplied by the water body. (correct)
  • Because the latent heat of vaporization is released into the water body.

Which of these statements is correct regarding water molecules during evaporation?

  • Water molecules are in constant motion, and adding heat increases their average speed. (correct)
  • Water molecules on the surface have varying, but consistent, velocities.
  • Water molecules are static within a body of water until heat is added.
  • The rate of evaporation decreases as the average speed of molecules increases.

Which of the processes is NOT directly involved with evaporation?

<p>Condensation. (A)</p> Signup and view all the answers

Consider a scenario where the temperature of a water body increases. How does this temperature change primarily influence evaporation?

<p>It increases the number of molecules with sufficient kinetic energy to escape. (C)</p> Signup and view all the answers

A pond is located in an area where the surrounding air becomes saturated with water vapor. How will this condition affect the rate of evaporation from the pond's surface?

<p>Evaporation rates will decrease as the air can hold less additional moisture. (A)</p> Signup and view all the answers

Assume two identical water bodies, A and B, are exposed to different environmental conditions. Water body A is exposed to a strong wind, while water body B is in a sheltered area with no wind. How will the wind affect the evaporation rate in water body A compared to water body B?

<p>Evaporation rate will be higher in water body A because the wind removes water vapor, maintaining a vapor pressure difference. (D)</p> Signup and view all the answers

If the latent heat of vaporization were significantly lower than its current value of approximately 585 cal/g, how would this change impact evaporation rates?

<p>Evaporation rates would increase because less energy would be needed for water molecules to change phase. (D)</p> Signup and view all the answers

In an aquifer with a storage coefficient (S) of $1.54 \times 10^{-3}$, if the portion due to water expansibility is 2.28%, what characteristic of the aquifer allows us to consider this contribution negligible?

<p>The aquifer is relatively incompressible, meaning the skeleton matrix dominates storage behavior. (C)</p> Signup and view all the answers

For a confined aquifer, how does the transmissibility (T) relate to the aquifer's permeability (K) and saturated thickness (b)?

<p>T = Kb, Transmissibility is directly proportional to both permeability and saturated thickness. (D)</p> Signup and view all the answers

How would you characterize the relationship between saturated thickness (H) and transmissibility (T) in an unconfined aquifer?

<p>T increases linearly with H, as a greater saturated thickness allows for greater water flow. (C)</p> Signup and view all the answers

What conditions must be met for the transmissibility (T) of an aquifer to be equivalent to the flow capacity (Q)?

<p>The hydraulic gradient (i) and aquifer width (w) must both be equal to 1. (B)</p> Signup and view all the answers

Limestone formations typically exhibit lower compressibility compared to other aquifer types. If a limestone aquifer has $E_s ≈ 2 \times 10^5 kg/cm^2$ and a storage coefficient (S) of $5 \times 10^{-5}$, what does this suggest about the relative contributions of water and aquifer skeleton to the overall storage?

<p>Water contributes approximately 70% to the storage, while the aquifer skeleton contributes 30%. (B)</p> Signup and view all the answers

What is the primary reason for maintaining a specific entrance velocity (approximately 2.5 cm/sec) through the slots of a well screen?

<p>To avoid incrustation and corrosion at the openings. (B)</p> Signup and view all the answers

According to the assumptions of Dupuit's equations, which of the following aquifer characteristics is assumed?

<p>The aquifer is homogeneous, isotropic, and of infinite areal extent with constant thickness. (D)</p> Signup and view all the answers

A fully penetrating well, as considered in Dupuit's assumptions, implies which condition?

<p>The well's screen covers the entire saturated thickness of the aquifer. (D)</p> Signup and view all the answers

What type of flow is assumed in the derivation of Dupuit's equations?

<p>Radial, horizontal, and laminar flow. (B)</p> Signup and view all the answers

Under what condition might the assumptions of Dupuit's equations be most inaccurate?

<p>When the pumped water is primarily drawn from aquifer storage without recharge. (A)</p> Signup and view all the answers

In the context of groundwater flow, what does 'complete well efficiency' imply, as assumed by Dupuit?

<p>The water level inside the well is the same as the water level in the aquifer immediately outside the well. (D)</p> Signup and view all the answers

Why is the assumption of an 'infinitely small well' important in the Dupuit's equations?

<p>It simplifies the mathematical calculations by eliminating the need to account for wellbore storage. (C)</p> Signup and view all the answers

What is a key difference between the Theis equation and the Dupuit equations in analyzing well hydraulics?

<p>The Theis equation accounts for water released from aquifer storage, whereas the Dupuit equations assume no recharge. (C)</p> Signup and view all the answers

Why does a decrease in the volume of water in an evaporation pan induce an error in evaporation measurements?

<p>A smaller volume of water takes less time to heat up during the day and cool down at night, which affects evaporation rates. (B)</p> Signup and view all the answers

What is the primary principle behind the energy-budget method for determining lake evaporation?

<p>Applying the law of conservation of energy by analyzing incoming, outgoing, and stored energy. (D)</p> Signup and view all the answers

In the water budget method, which of the following variables are typically estimated rather than directly measured?

<p>Daily groundwater inflow ($V_{ig}$) and daily seepage outflow ($V_{og}$). (D)</p> Signup and view all the answers

Which of the following is a limitation of the water budget method for determining lake evaporation?

<p>It relies on estimations of variables that are difficult to measure directly, such as groundwater flow. (B)</p> Signup and view all the answers

In the water budget equation, $EL = P + (Vis - Vos) + (Vig + Vog) - \Delta S - TL$, which term represents the daily surface inflow into the lake?

<p>Vis (D)</p> Signup and view all the answers

Assuming transpiration losses are insignificant, which simplified form of the water budget equation would be most appropriate for estimating daily lake evaporation?

<p>$E_L = P + (V_{is} - V_{os}) - \Delta S$ (B)</p> Signup and view all the answers

If the daily precipitation (P) is 5 mm, surface inflow ($V_{is}$) is 10 $m^3$, surface outflow ($V_{os}$) is 7 $m^3$, the increase in lake storage ($\Delta S$) is 2 $m^3$, and other terms are negligible, what is the daily lake evaporation ($E_L$) using the water budget method (in $m^3$)?

<p>3 $m^3$ (D)</p> Signup and view all the answers

Which method requires consideration of incoming energy, outgoing energy, and energy stored in the water body?

<p>Energy-Budget Method (C)</p> Signup and view all the answers

Which factor has the LEAST influence on the storage coefficient ($S$) in an artesian aquifer?

<p>Expansibility of water. (D)</p> Signup and view all the answers

What is the typical range of the storage coefficient ($S$) for an artesian aquifer?

<p>0.00005 to 0.005 (B)</p> Signup and view all the answers

In the equation $\Delta GWS = A_{aq} \times \Delta GWT \text{ or } ps \times S \text{ or } S_y$, what does $A_{aq}$ represent?

<p>Involved area of the aquifer. (C)</p> Signup and view all the answers

If an alluvial basin of $50 \text{ km}^2$ experiences a groundwater table drop of 2 meters and $40 \times 10^6 \text{ m}^3$ of groundwater is pumped with no replenishment, what is the specific yield ($S_y$) of the aquifer?

<p>0.4 (D)</p> Signup and view all the answers

An artesian aquifer has a thickness of 50 m and a porosity of 0.20. If the bulk modulus of compression is $1500 \text{ kg/cm}^2$, which additional parameter is essential for estimating its storage coefficient, according to the provided equation?

<p>Modulus of compressibility of the soil grains (B)</p> Signup and view all the answers

If the specific yield of a soil is 0.22 and the specific retention is 0.10, what is the porosity of the soil?

<p>0.32 (C)</p> Signup and view all the answers

A confined aquifer is characterized by which of the following properties regarding its storage coefficient ($S$)?

<p>It results from compressibility of the aquifer and expansibility of water. (A)</p> Signup and view all the answers

The change in groundwater storage ($\Delta GWS$) in an aquifer is MOST directly influenced by:

<p>The involved area of the aquifer, fluctuation in GWT/piezometric Surface, and the storage coefficient. (B)</p> Signup and view all the answers

How does the method for calculating changes in groundwater storage differ between confined and unconfined aquifers, according to the text?

<p>Confined aquifers use the storage coefficient, while unconfined aquifers use specific yield. (D)</p> Signup and view all the answers

Which statement best explains the relationship between porosity, specific yield, and specific retention in an aquifer?

<p>Porosity is the sum of specific yield and specific retention. (D)</p> Signup and view all the answers

According to Dalton's Law of Evaporation, what condition must be met for evaporation to cease?

<p>The saturation vapor pressure (𝑒𝑤) equals the actual vapor pressure in the air (𝑒𝑎). (B)</p> Signup and view all the answers

Why might two lakes with the same mean monthly air temperature exhibit different rates of evaporation?

<p>Other factors like wind speed, water temperature, and atmospheric pressure also influence evaporation. (D)</p> Signup and view all the answers

What happens when wind velocity is large enough to remove all evaporated water vapor?

<p>Any further increase in the wind velocity does not influence the evaporation. (B)</p> Signup and view all the answers

How does a decrease in barometric pressure affect evaporation, assuming other factors remain constant?

<p>It increases evaporation. (C)</p> Signup and view all the answers

Why does water with dissolved solutes generally evaporate at a slower rate than pure water?

<p>The solutes lower the water's vapor pressure. (C)</p> Signup and view all the answers

If seawater has a specific gravity 2.5% greater than pure water under identical conditions, approximately how much less evaporation would you expect from seawater compared to freshwater?

<p>2-3% (B)</p> Signup and view all the answers

Consider a shallow pond and a deep lake in the same geographical area. Which statement best describes their heat storage capabilities and impact on evaporation?

<p>The deep lake has more heat storage, potentially influencing its evaporation rate over time. (C)</p> Signup and view all the answers

A scientist observes that increasing wind speed over a large lake initially increases evaporation, but beyond a certain point has no additional effect. What best explains this observation?

<p>A critical wind speed value is reached, beyond which any further increase in wind speed has no influence on the evaporation rate. (C)</p> Signup and view all the answers

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Flashcards

Vapor Pressure

Pressure exerted by water vapor in equilibrium with its liquid phase.

Dalton’s Law of Evaporation

Rate of evaporation is proportional to the difference between saturation and actual vapor pressure.

Rate of Evaporation (EL)

Amount of water evaporated, measured in mm/day, influenced by vapor pressures.

Effect of Temperature on Evaporation

Higher water temperature increases evaporation rate; air temperature has less direct influence.

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Wind and Evaporation

Wind enhances evaporation up to a point; critical wind speed limits further increases.

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Barometric Pressure's Effect

Lower barometric pressure increases evaporation, especially at high altitudes.

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Effect of Soluble Salts

Dissolved salts reduce evaporation rate compared to pure water, linked to specific gravity.

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Heat Storage in Water Bodies

Deep water holds more heat than shallow water, affecting evaporation rates.

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Evaporation

The process where liquid changes to gas at temperatures below boiling through heat transfer.

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Hydrologic Cycle

The continuous movement of water on, above, and below the surface of the Earth.

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Kinetic Energy

The energy possessed by particles in motion, affecting evaporation rates.

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Latent Heat of Vaporization

The amount of heat energy required to convert 1 gram of liquid to gas without temperature change.

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Factors Affecting Evaporation

Various elements like temperature, humidity, wind speed, and surface area that influence evaporation rates.

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Measurement of Evaporation

Techniques and tools used to quantify the rate of evaporation from surfaces.

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Cooling Process

The effect that evaporation has on cooling the remaining liquid as heat is absorbed.

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Open Water Evaporation

Evaporation that occurs from bodies of water such as ponds or lakes.

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Bulk Modulus of Elasticity

A measure of a substance's resistance to uniform compression, quantified for water as 2.4 × 10⁴ kg/cm².

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Storage Coefficient (S)

A dimensionless value representing the amount of water stored or released per unit change in hydraulic head, calculated as S = 1.54 × 10⁻³ from the provided formula.

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Transmissibility (T)

The ease with which water can move through an aquifer, calculated as T = Kb in confined aquifers and T = KH in unconfined aquifers.

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Confined Aquifer

An aquifer sandwiched between impermeable layers, where transmissibility is independent of the piezometric surface.

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Unconfined Aquifer

An aquifer with a water table that is open to the atmosphere, where transmissibility is affected by the depth of the groundwater table (GWT).

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Evaporation Measurement

The process of assessing the amount of water lost due to evaporation from a surface.

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Water Budget Method

A simple method to estimate lake evaporation using the hydrological continuity equation.

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Hydrological Continuity Equation

An equation representing the balance of water entering and leaving a lake over time.

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Variables in Water Budget

Factors like precipitation and inflow/outflow that influence lake water volume.

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Energy-Budget Method

Estimation of evaporation based on incoming, outgoing, and stored energy.

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Transpiration Losses

Water loss from a lake due to plant processes, often considered minimal.

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Daily Average Values

Consistent measurements of variables calculated over a day for accurate assessment.

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Estimated Quantities

Values that cannot be measured directly, often requiring approximation.

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Entrance Velocity

The speed at which water enters through the slots of a well screen, typically around 2.5 cm/sec.

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Open Area Percentage

The fraction of the screen area that is open, usually between 15% to 18%.

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Dupuit’s Equations Assumptions

Key assumptions for deriving Dupuit's equations regarding aquifer behavior and flow.

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Stabilized Drawdown

The condition where pumping has created a constant water level in the aquifer over time.

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Artesian Aquifer

A groundwater aquifer with water under pressure, causing it to rise in wells.

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Homogeneous Aquifer

An aquifer with uniform properties throughout, such as permeability and thickness.

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Specific Weight of Water (γw)

The weight of water per unit volume, typically 9.81 kN/m³.

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Laminar Flow

A type of fluid flow in which water moves in parallel layers, allowing Darcy's law to apply.

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Transitional Flow Conditions

Flow conditions that occur when water is pumped from storage, causing drawdown to increase over time.

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Porosity (n)

The ratio of void spaces in soil or rock to the total volume.

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Theis Equation

An equation used to analyze unsteady radial flow into a well, considering water release from storage.

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Thickness of Confined Aquifer (b)

The vertical extent or thickness of a confined aquifer.

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Bulk Modulus of Water (Kw)

The measure of water's resistance to compression under pressure.

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Specific Yield (Sy)

The amount of water that can be drained from an unconfined aquifer per unit area and change in groundwater level.

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Specific Retention (Sr)

The amount of water retained in an aquifer after drainage, expressed as a fraction of the total volume.

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Change in Ground Water Storage (ΔGWS)

The difference in the volume of groundwater stored over time.

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Piezometric Surface (ps)

The imaginary surface that represents the height to which water would rise in tightly cased wells.

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Study Notes

Preface

  • This module provides a clear and detailed presentation of hydrology.
  • It covers the hydrologic cycle and processes like precipitation, evaporation, infiltration, overland flow, groundwater flow, and surface runoff generation.
  • The module was developed considering COVID-19 pandemic comments and suggestions from peers and faculty to ensure quality.

Unit 5: Evaporation

Intended Learning Outcomes

  • Define evaporation.
  • Identify factors affecting evaporation and measurement methods.
  • Identify methods for estimating evaporation from open water.

Introduction

  • Evaporation is a major hydrological process.
  • This chapter explains the physics of evaporation, factors influencing it, and methods to measure and estimate evaporation from open water sources.

Topics

Physics of Evaporation

  • Evaporation is a process where a liquid changes to a gas below the boiling point, transferring heat energy.
  • Water molecules move constantly, and some gain sufficient kinetic energy to cross the water surface.
  • The escaping water molecules form water vapor.
  • Evaporation is a cooling process as it requires heat energy.

Factors Affecting Evaporation

  • Vapor Pressure: The rate of evaporation is proportional to the difference between saturation vapor pressure and actual vapor pressure.
  • Temperature: Increased water temperature increases evaporation rate.
  • Wind: Greater wind velocity increases evaporation by removing the evaporated water vapor.
  • Atmospheric Pressure: Lower barometric pressure (higher altitude) increases evaporation.
  • Soluble Salts: Solutes in water reduce evaporation rate.
  • Heat Storage: Deeper water bodies have more heat storage, affecting seasonal evaporation.

Unit 5: 5.2.3 Measurements of Different factors for Evaporation

  • Lysimeter: A device to measure evapotranspiration by plants (usually crops or trees), recording precipitation and changes in soil moisture.
  • Types of lysimeters: weighable and non-weighable.
  • Weighable lysimeters are more expensive but provide precise short-term evapotranspiration estimates.
  • Non-weighable lysimeters are used for long-term measurements.
  • Pan Evaporation: It combines various climate factors like temperature, humidity, rainfall, solar radiation, and wind.
  • This method is useful for understanding how much water crops need for varying weather conditions.
  • A standard evaporation pan (like the USWB Class A pan) is used for consistent measurements.

Unit 6: Basic Subsurface Flow

Intended Learning Outcomes

  • Explain Darcy's Law, confined, and unconfined aquifers.
  • Solve problems related to groundwater confined/unconfined aquifers and Darcy's Law.

Introduction

  • Subsurface flow (formerly known as hypodermic flow) is part of the infiltrated rainfall.
  • It flows horizontally in the upper soil layers and appears at the surface.
  • Subsurface flow in water-bearing formations has a slower drainage rate than superficial flows but faster than groundwater flows.
  • It is dominant in humid regions with vegetated land surfaces.

Topics

Darcy's Law

  • Darcy's law states that the velocity of flow in a porous medium is proportional to the hydraulic gradient.
  • The formula for the flow rate is Q = KAI.

Confined and Unconfined Aquifers

  • An aquifer is a water-bearing geological formation transmitting water quickly, a valuable source for well extraction.
  • An aquiclude is a formation that absorbs water but doesn't transmit water significantly.
  • An aquifuge does not absorb or transmit water.
  • An aquitard transmits water slowly compared to an aquifer.
  • Specific Yield, is the volume of water draining through gravity
  • Specific Retention, is the percentage volume not drained by gravity
  • A water-table aquifer has a water table that forms the upper boundary.
  • A confined aquifer sits between two impermeable layers (aquicludes) under pressure.

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Explore evaporation as a key hydrological process. This module defines evaporation, identifies affecting factors, measurement methods, and estimation techniques from open water sources. Understand the physics behind evaporation and the energy transfer involved.

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