Sedimentation in the Nile River

Similar documents
Using Earth Observation Data for Monitoring River Basins

DROUGHT INDICES BEING USED FOR THE GREATER HORN OF AFRICA (GHA)

Analysis of Sedimentation in Wonogiri Reservoir

Climate also has a large influence on how local ecosystems have evolved and how we interact with them.

Sediment in the Nile River System

Tarbela Dam in Pakistan. Case study of reservoir sedimentation

AN ASSESSMENT OF THE RELATIONSHIP BETWEEN RAINFALL AND LAKE VICTORIA LEVELS IN UGANDA

Suspended sediment yields of rivers in Turkey

I C P A C. IGAD Climate Prediction and Applications Centre Monthly Climate Bulletin, Climate Review for April 2018

Subcommittee on Sedimentation Draft Sediment Analysis Guidelines for Dam Removal

El Nino 2015 in South Sudan: Impacts and Perspectives. Raul Cumba

THE STATE OF SURFACE WATER GAUGING IN THE NAVAJO NATION

Rong Jiang. Map of River. Table of Basic Data. China 14. Serial No. : China-14

Summary. Streams and Drainage Systems

I C P A C. IGAD Climate Prediction and Applications Centre Monthly Climate Bulletin, Climate Review for September 2017

I C P A C IGAD Climate Prediction & Applications centre

Earth Science Chapter 6 Section 2 Review

Mekong Sediment from the Mekong River Commission Study

How Do Human Impacts and Geomorphological Responses Vary with Spatial Scale in the Streams and Rivers of the Illinois Basin?

1. INTRODUCTION 2. HIGHLIGHTS

Illinois State Water Survey Division

River Response. Sediment Water Wood. Confinement. Bank material. Channel morphology. Valley slope. Riparian vegetation.

ICPAC. IGAD Climate Prediction and Applications Centre Monthly Bulletin, May 2017

Fenhe (Fen He) Map of River. Table of Basic Data. China 10

National Hydrology committee of Afghanistan (NHCA) Sedimentation in Reservoire

SPECIFIC DEGRADATION AND RESERVOIR SEDIMENTATION. By Renee Vandermause & Chun-Yao Yang

GAMINGRE 8/1/ of 7

WATER AVAILABILITY ASSESSMENT IN SHIPRA RIVER

Influence of the Major Drainages to the Mississippi River and Implications for System Level Management

CASE STUDY NATHPA JHAKRI, INDIA

The SedAlp Project: WP6: INTERACTION WITH STRUCTURES

Application of Real-Time Rainfall Information System to CSO control. 2 October 2011 Naruhito Funatsu METAWATER Co., Ltd.

Unconventional Wisdom and the Effects of Dams on Downstream Coarse Sediment Supply. Byron Amerson, Jay Stallman, John Wooster, and Derek Booth

CASE STUDY NATHPA JHAKRI, INDIA

A STUDY OF LOCAL SCOUR AT BRIDGE PIERS OF EL-MINIA

September 2016 No. ICPAC/02/293 Bulletin Issue October 2016 Issue Number: ICPAC/02/294 IGAD Climate Prediction and Applications Centre Monthly Bulleti

Bank Erosion and Morphology of the Kaskaskia River

CASE STUDY BINGA, PHILIPPINES

Application of SWAT Model to Estimate the Runoff and Sediment Load from the Right Bank Valleys of Mosul Dam Reservoir

UNIVERSITY OF CAMBRIDGE INTERNATIONAL EXAMINATIONS International General Certificate of Secondary Education

3/3/2013. The hydro cycle water returns from the sea. All "toilet to tap." Introduction to Environmental Geology, 5e

Analysis of Historical Pattern of Rainfall in the Western Region of Bangladesh

Flood Inundation Mapping under different climate change scenarios in the upper Indus River Basin, Pakistan

DROUGHT IN MAINLAND PORTUGAL

WATER ON AND UNDER GROUND. Objectives. The Hydrologic Cycle

In the space provided, write the letter of the description that best matches the term or phrase. a. any form of water that falls to Earth s

CLIMATE RESILIENT ALTITUDINAL GRADIENTS (CRAGs)

An investigation on the impacts of density currents on the sedimentation in dam reservoirs using TCM model; case study: Maroon dam

Dam Removal Analysis Guidelines for Sediment

Webinar and Weekly Summary February 15th, 2011

Floods Lecture #21 20

Science EOG Review: Landforms

Huong River. Serial No. : Viet Nam-8 Location: Thua Thien Hue Province, Viet Nam N 16 00' '

Climate Change: bridging scientific knowledge and public policy. Forum Parliament House, Canberra 18 March 2010

a) Name the features marked P,Q, and R b) Differentiate between a normal faulty and a reverse fault. 2. Use the diagram below to answer question (a)

STUDY GUIDE FOR CONTENT MASTERY. Surface Water Movement

Restoration Goals TFG Meeting. Agenda

The Colorado Drought of 2002 in Perspective

THE CONTEXT. Facts about Water, Erosion & Sedimentation

El Nino 2015: The Story So Far and What To Expect Next

The effectiveness of check dams in controlling upstream channel stability in northeastern Taiwan

El Nino 2015: The Story So Far and What To Expect Next

Learning Objectives: I can identify and interpret river flows and directions.

NREM 407/507 April Jordan River today Danube on Tuesday. 2. Quiz. 3. Discuss Stream Bank Stabilization

GEOL 1121 Earth Processes and Environments

Morphological Changes of Reach Two of the Nile River

Cambridge International Examinations Cambridge International General Certificate of Secondary Education

Strategies for managing sediment in dams. Iwona Conlan Consultant to IKMP, MRCS

Numerical modeling of sediment flushing from Lewis and Clark Lake

A "consensus" real-time river flow forecasting model for the Blue Nile River

Behavior of radioactive cesium accumulation in water bodies in contaminated area by FDNPP accident

Water Management for Environmental Restoration Flows In the Big Bend reach, Rio Grande Rio Bravo

CASE STUDY BINGA, PHILIPPINES

Chapter 11. Rivers: Shaping our landscape

Technical Memorandum No

SUSTAINABLE SEDIMENT MANAGEMENT

IGAD Climate Prediction and Applications Centre Monthly Bulletin, August 2014

Proposal to limit Namakan Lake to 1970 Upper Rule Curve for remainder of summer

Soil Erosion Calculation using Remote Sensing and GIS in Río Grande de Arecibo Watershed, Puerto Rico

GTU. Shantilal Shah Engineering College, Bhavnagar

Surface Water Short Study Guide

Recent changes of suspended sediment yields in the Upper Yangtze River and its headwater tributaries

Flash flood disaster in Bayangol district, Ulaanbaatar

Sediment and nutrient transport and storage along the urban stream corridor

Attachment B to Technical Memorandum No.2. Operations Plan of Ross Valley Detention Basins

REDWOOD VALLEY SUBAREA

Integrating Weather Forecasts into Folsom Reservoir Operations

IGAD Climate Prediction and and Applications Centre Monthly Bulletin, August May 2015

MARMOT CREEK BASIN: MANAGING FORESTS FOR WATER

SOCIO-ECONOMIC IMPACTS OF FLOODING IN DIRE DAWA, ETHIOPIA

Written Response Test

CHANGES OF RUNOFF MECHANISM OF THE BRANTAS RIVER OVER THE PAST 30 YEARS

CR AAO Bridge. Dead River Flood & Natural Channel Design. Mitch Koetje Water Resources Division UP District

Nile Basin Reservoir Sedimentation Prediction and Mitigation

2015 Fall Conditions Report

and the Myanmar economy World Water Day, 2018

Stone Outlet Sediment Trap

WIND EFFECTS ON CHEMICAL SPILL IN ST ANDREW BAY SYSTEM

SCOPE OF PRESENTATION STREAM DYNAMICS, CHANNEL RESTORATION PLANS, & SEDIMENT TRANSPORT ANALYSES IN RELATION TO RESTORATION PLANS

CASE STUDY SOLIS, SWITZERLAND

Transcription:

Advanced Training Workshop on Reservoir Sedimentation Sedimentation in the Nile River Prof. Dr. Abdalla Abdelsalam Ahmed 10-16 Oct. 2007, IRTCES, Beijing, China CWR,Sudan 1

Water is essential for mankind survival and the development of civilizations. The population of the world continues to increase by 100 million people each year, with a corresponding demand of water. Environmental pollution and water contamination make the situation very critical. Sediment, among its many advantages and disadvantages, is considered one of the main water pollutant factor. CWR,Sudan 2

Sedimentation impacts Sedimentations has its impacts on the utilization of the Nile Basin water resources, ranging from watershed degradation, sediment deposition in reservoirs to management difficulties of irrigation canals networks. CWR,Sudan 3

General Layout of the Nile Basin CWR,Sudan 4

Nile River receives its flow from three main distinct watersheds:- I. Equatorial lakes plateau in the South. II. Sudd region in the Center. III. Ethiopian Highlands in the East. CWR,Sudan 5

Eastern Main Watershed Central Watershed Southern Watershed Main Watersheds of Nile River Basin CWR,Sudan 6

The share and distribution of the 10 riparian countries to the Nile N River Country Total area of the country (km2) As % of total area of basin Burundi Rwanda Tanzania Kenya DR Congo Uganda Ethiopia Eritrea Sudan Egypt Nile basin 27 834 26 340 945 090 580 370 2 344 860 235 880 1 100 010 121 890 2 505 810 1 001 450 8889 534 0.4 0.6 2.7 1.5 0.7 7.4 11.7 0.8 63.6 10.5 100.0 CWR,Sudan 7

Atbra River Khartoum Cross-section of the Nile River from Equatorial Source to Drain CWR,Sudan 8

1000 Nile River Hydrograph CWR,Sudan 9

The process of sedimentation usually happens in the following stages Erosion Entrainment (drawing of particles into fluid) Transportation Compaction or/and Consolidation (deposition) CWR,Sudan 10

The amount and rate of deposit are determined mainly by:- i. Detention storage time. ii. The shape of the reservoir. iii. The operating procedure of the reservoir. iv. The depositional pattern usually starts with the coarser material depositing towards the reservoir headwater. The aggradations continues more and more until a delta is formed, as it happens in Roseires reservoir in the Blue Nile (Sudan) and Aswan High Dam reservoir in the Main Nile (Egypt). CWR,Sudan 11

Causes of sediment in watersheds can be summarized as follows:- Removal of forests or other vegetation sharply reduces water retention and increases erosions resulting in reduced water availability in dry seasons and more sedimentation downstream. Absence of trees provides bad effects on shrubs which lost shelters and some times die out under burning sun. Charges in river flow, sediment and pollutant loadings resulting from activities for inland degrade downstream ecosystem. Dams are the worst hit by sedimentation. CWR,Sudan 12

Nile River Sediment Most of the sediment in the Nile flows from the Ethiopian Highlands through the Blue Nile and Atbara River. The White Nile and its tributaries lose most of its sediment load by spilling and deposition over flood plains, lakes and marshlands inside Sudan. Nearly all of the sediment (~ 90%) comes from the Blue Nile during the flood season (July- Oct.) The sediment load of the Blue Nile at El Diem is 140 million tons per year. The sediment load at Aswan High Dam was 160 million tons taking into consideration the amount of sediment transported by Atbara River. CWR,Sudan 13

This is compared to 150 Million tons for Mississippi River, 250 Million tons the Colorado River and 2000 (1600) Million tons for Yellow River in China. there is no reliable means of bed load information in the Nile River. However, the bed load is believed to be negligible. The coarser sand usually deposits in the upper portion of the Blue Nile near the Ethiopian/Sudanese boarder. The lighter sediment is carried by the flow to the downstream. The suspended sediment load distribution is 30% clay (<0.002 mm), 40% silt (0.002 0.02 mm) and 30% fine sand (0.02 0.2 mm). Therefore, it may be considered in general wash load. CWR,Sudan 14

Total Annual Sediment Load (million tons) in The Nile River CWR,Sudan 15

Comparison of rainfall, Discharge and Sediment Yield in the River Atbara Comparison of Rainfall, Discharge and Sediment Yield in the Blue Nile CWR,Sudan 16

60.00 50.00 Sediment Concentration (mlg/litre) 40.00 30.00 20.00 10.00 0.00 JAN FEB. MAR. APR. MAY JUN. JUL AUG. SEP. OCT. NOV. DEC. Months Suspended Sediment Concentration in AHD Reservoir CWR,Sudan 17

Impacts on Downstream Countries Here in Sudan the problem has been reflected downstream in terms of sediment deposition in the reservoirs and the irrigation canalization networks, causing: flood risks crops damage pumps intakes blockage low production hydropower generation difficulties CWR,Sudan 18

Sediment Volume and Content of Sennar Dam CWR,Sudan 19

The Data Dam Wall Debris Dam Wall Delta Formation Upstream, Roseries Dam Debris in the Reservoir Upstream, Roseries Dam CWR,Sudan 20

Reservoir Sedimentation Sennar dam in 61 years lost 71% (660 million m 3 ) of its original reservoir capacity. In the first ten years the drop in the capacity of Roseires dam was 550 millions m 3 with a rate of 55 Mm 3 per year. In the second period (1976-1981) the reduction in the capacity was 100 Mm3 with a rate of 20 Mm3 per year. In the period (1981-1985) the reduction in the capacity was 120 Mm 3 with a rate of 30 Mm 3 per year. However, a drastic increase in the sedimentation rate occurred in the period (1985-1992) with a rate of 60 Mm3 per year and a reduction of 427 Mm3. CWR,Sudan 21

Irrigation Difficulties due to Sedimentation - Gezira Scheme - Sudan Sediment Excavated from the Canal Sediment Excavated from the Canal Inadequate Sedimentation Clearance CWR,Sudan 22

Sediment Socio-economic and Environment Impacts Changes in sediment quantity and quality can have a significant impact on a range of social, economic and environmental systems. The deposition of sediment in irrigation canals and its subsequent built-up of aquatic weeds results in losses in production of great magnitude. The cost of sedimentation includes loss of hydropower potential. The most serious effect, is the loss of agricultural production. In Sudan the sediment clearance from the irrigation canalization system costs more than 60% of the total cost of the operation and maintenance. CWR,Sudan 23

Conclusions The sedimentation in the reservoir and the irrigation systems within the Nile Basin has environmental and socio-economic impacts. Suitable sedimentation management is a key for the sustainable water resources management. Changes in human activities within the catchment can have detrimental effects on both sediment quantity and quality. It is very important to evaluate environmental impacts involved in sediment management properly and mitigate them as much as possible. Sedimentation rate in the last decade (1990s) increased rapidly, indicating that huge and wide land degradation is occurring in the catchment area of the Nile River system. Integrated sediment management is found to be the best policy to minimize the adverse impacts of the sedimentation within the entire Nile River Basin. CWR,Sudan 24

Thank you for your attention CWR,Sudan 25