This training was prepared by the U.S. Department of Agriculture (USDA) team of Otto Gonzalez-USDA Foreign Agricultural Service (Team Leader), Jon Fripp.

Slides:



Advertisements
Similar presentations
The Middle and Lower Course of a River
Advertisements

How Do Rivers Change the Land?
Introduction to Windbreaks This training was prepared by the U.S. Department of Agriculture (USDA) team of Otto Gonzalez-USDA Foreign Agricultural Service.
This training was prepared by the U.S. Department of Agriculture (USDA) team of Otto Gonzalez-USDA Foreign Agricultural Service (Team Leader), Jon Fripp.
Introduction to Surface Irrigation
This training was prepared by the U.S. Department of Agriculture (USDA) team of Otto Gonzalez-USDA Foreign Agricultural Service (Team Leader), Jon Fripp.
Grade Control Structures Chris Shrimpton and Jonathan McIntosh CIVE 717 River Mechanics Spring 2012.
Chapter 13 Worksheets Section 1-4.
Introduction to Stone (riprap) Protection
River Studies. Outline of Events During your river field work you will be visiting two different sites in the lower course of the river. At each site.
Water Erosion Chapter 3 Section 2.
Natural Riparian Resources Vegetation Landscape/Soil Water.
Surface Water Topics: Surface Water Movement Stream Development
EARTH SCIENCE Geology, the Environment and the Universe
Objectives Describe how surface water can move weathered materials.
RIVER FORMATION EARTH’S GRAVITATIONAL FORCE PULLS OBJECTS TOWARD IT’S CENTER OF MASS. WATER FALLING DOWN A SLOPE IS EVIDENCE OF GRAVITY. AS OBJECTS DROP.
Chapter 6 Section 1 – Running Water
This training was prepared by the U.S. Department of Agriculture (USDA) team of Otto Gonzalez-USDA Foreign Agricultural Service (Team Leader), Jon Fripp.
Watershed Zone 2 Kabul, 2006 This training was prepared by the U.S. Department of Agriculture (USDA) team of Sarah Librea-USDA Foreign Agricultural Service.
Seedbed and Seed drill This training was prepared by the U.S. Department of Agriculture (USDA) team of Sarah Librea-USDA Foreign Agricultural Service (Development.
Introduction to Planting In Dry Areas This training was prepared by the U.S. Department of Agriculture (USDA) team of Sarah Librea-USDA Foreign Agricultural.
HEC-RAS US Army Corps of Engineers Hydrologic Engineering Center
This training was prepared by the U.S. Department of Agriculture (USDA) team of Sarah Librea-USDA Foreign Agricultural Service (Team Leader), Jon Fripp.
This training was prepared by the U.S. Department of Agriculture (USDA) team of Otto Gonzalez-USDA Foreign Agricultural Service (Team Leader), Jon Fripp.
This training was prepared by the U.S. Department of Agriculture (USDA) team of Sarah Librea-USDA Foreign Agricultural Service (Development Resources Specialist),
This training was prepared by the U.S. Department of Agriculture (USDA) team of Otto Gonzalez-USDA Foreign Agricultural Service (Team Leader), Jon Fripp.
This training was prepared by the U.S. Department of Agriculture (USDA) team of Otto Gonzalez-USDA Foreign Agricultural Service (Team Leader), Jon Fripp.
Erosion and Deposition
Chapter 13 Surface Water.
Natural Riparian Resources Water Landscape & SoilVegetation.
Lesson 9 Channel characteristics
This training was prepared by the U.S. Department of Agriculture (USDA) team of Otto Gonzalez-USDA Foreign Agricultural Service (Team Leader), Jon Fripp.
River processes Learning objectives: 1.Understand the different types of weathering 2.Know what mass movement is 3.Understand the different types of erosion.
River Systems Earth Space Science Mr. Coyle. The Hydrologic Cycle Infiltration = Groundwater System Runoff = Surface Water System Runoff = Precipitation.
 This will occur when streams receive more water than their channels can hold,  i.e. when stream discharge is greater than stream capacity.  Streams.
Measuring velocity profiles above different substrates on the Glinščica stream Maja Koprivšek 1, Mitja Brilly 1, Mihael Jožef Toman 2 1 University of Ljubljana,
Introduction to Spring Development
Fresh Water Chapter 7 Sections 1-4 SOL 6.7. Earth is called the “water planet” because nearly ¾ of Earth is made up of water. 97% salt water 3% fresh.
This training was prepared by the U.S. Department of Agriculture (USDA) team of Otto Gonzalez-USDA Foreign Agricultural Service (Team Leader), Jon Fripp.
13.1 Streams and Rivers Key Idea:
Rivers and Streams. River Systems A river or stream: any body of water flowing downhill in a well defined channel A river or stream: any body of water.
This training was prepared by the U.S. Department of Agriculture (USDA) team of Otto Gonzalez-USDA Foreign Agricultural Service (Team Leader), Jon Fripp.
River Systems. Objective  Students will describe factors that affect the erosive ability of a river and the evolution of a river system.
Introduction to the Advantages of Vegetation
11.1 The Active River. Do you think a river can have a source? Describe where you would expect to find a river’s source. The source of a river is where.
Bitter Creek Stream Restoration Preliminary Engineering Report Neighborhood Meeting.
Natural Riparian Resources Vegetation Landscape/Soil Water.
Power of a Rain drop.
River Systems You will learn: Where do rivers begin?
Fresh Water.
11.1 The Active River.
Rivers & Groundwater.
Freshwater Systems less than 1% of the water on Earth is available for us as freshwater freshwater exists as surface water groundwater.
Fresh Water Chapter 7 Sections 1-4 SOL 6.7.
Meandering Rivers.
Rural – land degradation in a semi-arid
Rivers & Groundwater.
1ST YEAR OF ESO RIVERS PROFESOR TIERNO GALVÁN SECONDARY SCHOOL.
Introduction to Agriculture, Food, and Natural Resources
Where Does the “Stuff” Go?
The Flow of Freshwater.
Rural – land degradation in a semi-arid
Changes in a river from source to mouth
Running Water Earth Science Chapter 6
Prentice Hall EARTH SCIENCE
HEC-RAS US Army Corps of Engineers Hydrologic Engineering Center
Where Does the “Stuff” Go?
Geography Knowledge Organiser: Year 7 Unit 6 – Rivers
Shaver Creek Permitting
Presentation transcript:

This training was prepared by the U.S. Department of Agriculture (USDA) team of Otto Gonzalez-USDA Foreign Agricultural Service (Team Leader), Jon Fripp (Civil Engineer) and Chris Hoag (Wetland Plant Ecologist)-USDA Natural Resources Conservation Service (Civil Engineers). Fripp and Hoag were the primary authors of this material. The U.S. AID provided funding support for the USDA team. 8 Introduction to Check Dams

Check Dams Usually Used in Collection Zone Can Also be used in Transport Zone

These are structures Use caution Understand the processes at work in the system Know the components of a check dam !

What happens in if all the vegetation is removed from a watershed? Understand the processes at work in the system Answer: More erosion of surface

So what happens if you have more water running down the watershed collection zone? Answer: Erosion. Gullies will form and grow. The channel will get hungry and eat its boundary.

The stream or gulley will start by attacking the bottom of the channel first.

The channel will get deeper Section

The channel will keep getting deeper until the sides start to fall in Section

Then it starts to get wider Now it is really starting to get bad

This is process is called the channel stages Stage 1 Section Stage 3 Stage 2 Assessment Tool: Channel Stages Good for collection and transport zone

STAGE 1 Test Time

Headcut STAGE 2 Channel downcutting creates straighter, steeper gully.

widening STAGE 3 Channel widening, cut banks on both sides.

It is best to stop this process early in Stage 2

To stop it: use a check dam Profile Stage 2

Profile A check dam will keep the channel from getting too deep

Check Dams Lots of different types Lots of different materials

A Check Dam must Have a Control Section Have a Energy Dissipation Section Be Keyed into Channel Bottom Be Keyed into Channel Bank Be appropriately spaced Components of a check dam This introduction is going to cover the basics You may want to get more detailed training

Control Section: Keeps the water in the channel Bank Key: Keeps water from eroding around check dam

Control Section should have the same area as a stable section of the stream or gully.

Energy dissipation section should be two times the structure height Maximum height should be less than 1.5 m H 2H

Key into channel bottom for a minimum of 60 cm Key into channel bank for a minimum of 1 m Top of check dam should be at least 30 cm below top of channel section 1 m 60 cm

Energy Dissipation Section: Absorbs energy as water flows over top. Key into Channel Bottom: Keeps water from eroding under check dam May need a filter with log check dams Profile Same rules for all types of check dams

Profile The check dams work as a team Downstream erosion might undermine the upstream check dam

Space so that the slope can be level between the check dams and the upstream one will not be undermined. Profile

Test Time Question: What is wrong with this check dam Answer: bank key and adjacent protection

Question: What is wrong with this check dam? Answer: no control section. Made worse by bad bank key

Question: What is wrong with this check dam? Answer: bank key in

Answer: everything, bad spacing, no control section, no bed or bank key in, no energy dissipation Question: What is wrong with this check dam?

Answer: nothing major

Question: What is wrong with this check dam? Answer: nothing major

Question: What is wrong with these check dams? Answer: nothing major

You need an engineer to help with the design if: The river has high velocities The river is large The erosion is significant The river system is unstable There is something very important on the bank The project will cost a lot of money Laws state you must have an engineer

The End