CE 3354 Engineering Hydrology Lecture 2: Surface and Groundwater Hydrologic Systems.

Slides:



Advertisements
Similar presentations
Hydrology Rainfall - Runoff Modeling (I)
Advertisements

Water Resources Water is essential to life on Earth. Humans can live for more than month without food, but we can live for only a few days without water.
Water Resources.
Introduction to Groundwater Flow Modeling Prof. Dr. Halil Önder Fall 2008.
Introduction to Physical and Chemical Hydrogeology (GEO 346C) Instructor: Bayani Cardenas TAs: Travis Swanson and John Nowinski
Dr. Nicolas Zegre Understanding the Hydrologic Cycle.
Groundwater The Unseen Part of the Water Cycle Salt Groundwater Ground Water Reservoir The present-day surface hydrologic cycle. The numbers in parentheses.
Hydrologic Cycle and Watersheds. Hydrologic Cycle Components Precipitation Infiltration Percolation Runoff Evapotranspiration.
CE 533 Groundwater Flow & Contaminant Transport Introduction and terminology.
Engineering Hydrology (ECIV 4323)
Watershed Hydrology, a Hawaiian Prospective; Groundwater Ali Fares, PhD Evaluation of Natural Resource Management, NREM 600 UHM-CTAHR-NREM.
Groundwater.
Hydrographs and Drainage Basins. Drainage Basins: A drainage basin is the catchment area of a river and its tributaries. The boundary of the catchment.
Quick review of remote sensing, Introduction to remote sensing in hydrology, hydrological cycle and energy balance Lecture 1.
EEOS 350: Quantitative hydrogeology Lecture 2 Water balance.
Workshop on Effective Implementation of IWMP
Applying Methods for Assessing the Costs and Benefits of CCA 2 nd Regional Training Agenda, 30 September – 4 October 2013 Priyanka Dissanayake- Regional.
The Islamic University of Gaza Faculty of Engineering Approaches to Groundwater Modeling Conceptual Model.
1 The Hydrologic Cycle Where is the water? The global cycle Groundwater –The myth of underground rivers.
Watershed Assessment and Diagnosis of Condition for August 20, 2007 Joe Magner and Greg Johnson MPCA.
GEO/ENV 315/GEO 514 Hydrogeology Class meets: Time: Mondays: 5:30 pm – 8:30 pm. Location: ESS 183 Office Hours: Wednesdays and Fridays 3:00 – 4:00 pm ESS.
Exam pt improvement over 1 st exam (better than past) 150 (63%) improved over the first exam.
 Last week we discussed how run-off can occur two different ways:  Surface Run-off – water flowing on the surface to streams, rivers and oceans.  Subsurface.
These notes are provided to help you pay attention IN class. If I notice poor attendance, fewer notes will begin to appear on these pages 1.
CE 424 HYDROLOGY 1 Instructor: Dr. Saleh A. AlHassoun.
Water Resources A river runs through it…. Water: The Universal Solvent One of the most valuable properties of water is its ability to dissolve. This makes.
Engineering Hydrology (ECIV 4323)
1 GROUNDWATER HYDROLOGY AND CONTAMINANT TRANSPORT CEVE 518 P.C. de Blanc C.J. Newell 1.Hydrologic Cycle and Water Distribution 2.Soil Horizons 3.Aquifers.
Water Resources.
11-1 Water Resources Page 269. A. The Water Cycle 1. Water is a renewable resource. Why?
Introduction to Water You need to write down the underlined words for vocabulary!
 Before break, we discussed watersheds and what constitutes a watershed. How do you think water moves through a watershed?
AOM 4643 Principles and Issues in Environmental Hydrology.
Water Resources Environmental Science Spring 2011.
CE 3354 Engineering Hydrology Lecture 21: Groundwater Hydrology Concepts – Part 1 1.
The Islamic University of Gaza Faculty of Engineering Civil Engineering Department EENV 5326 Groundwater Modeling.
Introduction to Water – Chapter 24. Pretest Water: 4 Primary Sections The Hydrologic Cycle (Water Cycle) The Hydrologic Cycle (Water Cycle) Glaciers.
The Hydrological Cycle
Water Cycle Animation Study Jams. Next > Humans depend on water. For this reason, throughout history, humans have settled near water sources. The most.
Hydrology & Climatology (including Geohydrology) Louisiana Department of Environmental Quality 2010 Envirothon Training.
Groundwater Geol 1110 Newell guest lecture 3/28/16.
Sanitary Engineering Lecture 4
Water Terms
Radial Flow to an Unconfined Aquifer From Mays, 2011, Ground and Surface Water Hydrology.
Runoff.
Groundwater Review Aquifers and Groundwater Porosity
Near-surface Geologic Environments
Chapter 3 The Conceptual Model
DES 606 : Watershed Modeling with HEC-HMS
Klamath ADR Hydrology Report
Engineering Hydrology (ECIV 4323)
The Global & Local Storage and Flow of Water
Test 1 Review Chapter 1, Hydrologic cycle and the water balance
2.3.2a Water Cycle, Surface Water, and Ground Water
Water Cycle It keeps cycling back
Groundwater & Aquifers
The Islamic University of Gaza Faculty of Engineering Approaches to Groundwater Modeling Conceptual Model.
2.3.2a Water Cycle, Surface Water, and Ground Water
2.1 Basic hydrology.
Groundwater.
Water Cycle It keeps cycling back
Hydrology CIVL341.
The hydrologic cycle.
Engineering Hydrology (ECIV 4323)
Aquifers, Groundwater, and Surface Water
Hydrology CIVL341 Introduction
Engineering Hydrology (ECIV 4323)
Match the drainage basin terms to the correct definitions!
The Hydrologic Cycle and Groundwater
Systems and Components – A Process for Developing the Total Water Budget Handbook for Water Budget Development - With or Without Models CWEMF 2019 Annual.
Presentation transcript:

CE 3354 Engineering Hydrology Lecture 2: Surface and Groundwater Hydrologic Systems

Outline Fundamental Definitions Water Budget Surface Water Systems Groundwater Systems

What is Hydrology? Study of the occurrence, circulation, storage, and distribution of surface and groundwater on the Earth. Engineering hydrology is the quantification of amounts of water at various locations (spatially) as a function of time (temporally) for surface water applications.

What is a Watershed? Topographic area from which water collects and discharges as surface streamflow through or past one point of interest (outlet, mouth, pour point, or engineering site). The area on the surface of the Earth that drains to a specific location In groundwater a similar concept is called a groundwater basin – only the boundaries can move depending on relative rates of recharge and discharge

Hydrologic Systems A hydrologic system is simply a collection of connected components that form the hydrologic cycle These components can be grouped into subsystems, treated separately, and the results combined according to interactions between the subsystems (CMM pg 5)

Hydrologic Cycle

Surface Water Component

Groundwater Component

As a System Diagram

Another View of Hydrologic Cycle

Water Budget The water budget, or hydrologic balance is simply the expression of the conservation of mass in hydrologic terms for a hydrologic system. Generally it is expressed as a rate (or volume) balance. The hydrologic equation is the fundamental tool in hydrology to describe amounts of water in storage in different compartments at different scales. The equation expressed in “words” is Rate of inflow - Rate of outflow = Rate of change of storage + Rate of internal mass generation.

Water Budget Compare to Equation in CMM; Except for notation, and absence of internal generation they equations are identical.

Surface Water Systems

Surface Water Budget From the surface water system diagram, an appropriate budget would be Inflows: Rainfall; Surface water from outside boundary, recharge from Groundwater. Outflows: Evapotranspiration; Surface water leaving boundary; Infiltration to groundwater. Storage: Water levels in lakes, rivers, ponds within the boundary; water stored on leaves and other surfaces.

Ground Water Systems

Ground Water Budget From the surface water system diagram, an appropriate budget would be Inflows: Groundwater flow from outside boundary; Recharge from surface system (via infiltration) Outflows: Groundwater flow out of the boundary; Discharge (pumping; springs) to surface system Storage: Water levels in aquifers within the boundary

The Combined System

Conceptual Model of Water Budget Infiltration (mm)

Water Budget Example

Aquifers An aquifer is a geologic formation that stores and transmits water Storage is in the interstitial (pore) space between the solid particles that comprise the formation Transmission is in the interconnected pore space

Porosity and Water Content

Types of Porous Structure

Moisture Zones

Aquifer Types

Summary Definitions Surface water system introduction Subsurface water system introduction Concept of a water balance Porous media and aquifers

Next Time Hydrologic Data Watershed Delineation