MOSE PROJECT AND HYDRO MORFOLOGICAL MONITORING IN THE VENICE LAGOON



Similar documents
SEA LEVEL REAL TIME MONITORING SYSTEM IN THE NORTHEASTERN ITALY

Waterfront Redevelopment: a Strategic factor of Urban Regeneration in Venice

Martin County Coastal GIS Program St Lucie Inlet Planning Tool

RESTORATION AND ENHANCEMENT OF SOUTHERN CALIFORNIA LAGOONS

The Integration of Hydrographic and Oceanographic Data in a Marine Geographic Information System U.S. Hydro 2015

Hydraulics Laboratory Experiment Report

Present measurement networks in Italy and future developments

2.0 BASIC CONCEPTS OF OPEN CHANNEL FLOW MEASUREMENT

Experiment (13): Flow channel

Waters of the State CALIFORNIA

Alimentatori LED LED drivers

Index-Velocity Rating Development (Calibration) for H-ADCP Real-Time Discharge Monitoring in Open Channels

Choices and Applications of 2D/3D models for supporting harbour & coastal management

CFD Modelling of a Physical Scale Model: assessing model skill. Kristof Verelst FHR, Antwerp

4.14 Netherlands. Interactive flood risk map of a part of the province of Gelderland in the Netherlands. Atlas of Flood Maps

Passenger Terminal Amsterdam

...Eq(11.6) The energy loss in the jump is dependent on the two depths y 1 and y 2 3 = E =...Eq(11.7)

Bolinas Lagoon Ecosystem Restoration Feasibility Project Marin County Open Space District

Monitoring and control of openchannel flow in irrigation canals

New Coastal Study for Puerto Rico FIRMs. Paul Weberg, FEMA RII Mat Mampara, Dewberry Jeff Gangai, Dewberry Krista Collier, Baker

Estimation of radial sea currents in the northern Adriatic Sea close to the Venice Lagoon inlets #ID2141

The World's Most Interesting Tourist Attractions

Catchment Scale Processes and River Restoration. Dr Jenny Mant The River Restoration Centre therrc.co.uk

Particle tracking-modeling of morphologic changes in the Ria de Aveiro

PREDICTING THE IMPACT OF CLIMATE CHANGE ON SALINITY INTRUSIONS IN COASTAL SOUTH CAROLINA AND GEORGIA

Field Data Recovery in Tidal System Using Artificial Neural Networks (ANNs)

ebb current, the velocity alternately increasing and decreasing without coming to

MIKE 21 FLOW MODEL HINTS AND RECOMMENDATIONS IN APPLICATIONS WITH SIGNIFICANT FLOODING AND DRYING

Exercise (4): Open Channel Flow - Gradually Varied Flow

Facing an Uncertain Future: Increasing Resilience at Marinas and Harbors. Recreational Boating Educational Conference December 11, 2014

A Case Study Documenting the Dubai Coastal Zone Monitoring Programme An International Example.

Damage Assessment in a large River Basin The Mekong Experience. Phan Nguyen& Anthony Green Mekong River Commission

What is the most obvious difference between pipe flow and open channel flow????????????? (in terms of flow conditions and energy situation)

Chapter 10. Flow Rate. Flow Rate. Flow Measurements. The velocity of the flow is described at any

MI oceanographic data

Delaware Integrated Marsh Monitor Network: Evaluating sedimentation and sea-levels effects on marsh surface elevation and evolution

Designing a Basic White Water Canoe/Kayak Course using InfoWorks ICM

The Geosites of the province of Venice

The Coast of Crystal Cove Orange County, California

TENNESSEE GAS PIPELINE COMPANY, L.L.C.

Gravir Outer, Isle of Lewis Site and Hydrographic survey report

Design And Construction Of The South San Diego Bay Western Salt Pond Restoration Project Headwaters To Ocean Conference

The extensive monitoring of suspended sediments by means of ultrasound (an ADCP application)

УДК 528 Nguyen Thanh Le APPLYING MULTIBEAM ECHO-SOUNDER SYSTEM IN MAKING MULTISCALE SEABED TOPOGRAPHY MAP IN VIETNAM

SITE INVESTIGATIONS OF THE BEACH EROSION PROBLEM AT MAHO BEACH, ST. MAARTEN

Persistent Scatterer Interferometry and Cosmo-SkyMed data in the Piano Straordianario di Telerilevamento Ambientale (PST-A) Salvatore Costabile

3.4 DRAINAGE PLAN Characteristics of Existing Drainages Master Drainage System. Section 3: Development Plan BUTTERFIELD SPECIFIC PLAN

Flood Mitigation and Management in Bangkok Metropolitan Area

Storm tide is the water level rise during a storm due to the combination of storm surge and the astronomical tide.

National Groundwater Conference Canberra, November 2010

CEE 370 Fall Laboratory #3 Open Channel Flow

Storm Drainage Systems

Abstract. 1 Introduction

Dr. Eng. Adamo, List of publications Page 1 of 5

Storm tide is the water level rise during a storm due to the combination of storm surge and the astronomical tide.

Consultation on integrating flood defence consents into the Environmental Permitting regime in England and Wales

1.0 INTRODUCTION 2.0 SCOPE OF WORK. DATE July 29, 2010 PROJECT No /2000

AirborneHydroMapping. New possibilities in bathymetric and topographic survey

Effect of barrages on water level in estuaries

Water Management in the Netherlands

FLOW CONDITIONER DESIGN FOR IMPROVING OPEN CHANNEL FLOW MEASUREMENT ACCURACY FROM A SONTEK ARGONAUT-SW

Procedia Environmental Science, Engineering and Management

Scour and Scour Protection

Numerical Investigation of Angle and Geometric of L-Shape Groin on the Flow and Erosion Regime at River Bends

Assessment of hydropower resources

Battery Thermal Management System Design Modeling

Automated In-Situ Water Quality Monitoring Report

CHAPTER 3 STORM DRAINAGE SYSTEMS

Rural Flooding: The Potential Role of Forestry

Active and Passive Microwave Remote Sensing

Section 401 Water Quality Certification

Head Loss in Pipe Flow ME 123: Mechanical Engineering Laboratory II: Fluids

Physical Modeling and CFD Simulation of Wave Slamming on Offshore Wind

Training programme on flow measurements

Delta development. Teunis Louters Delta Development, the Netherlands

5.0 OVERVIEW OF FLOOD DAMAGE REDUCTION MEASURES

The Alternatives of Flood Mitigation in The Downstream Area of Mun River Basin

SECTION 6A STORM DRAIN DESIGN Mar S E C T I O N 6A STORM DRAIN - DESIGN

U.S. Fish and Wildlife Service will invest $15 million for post-sandy cleanup and marsh restoration on Long Island

A water quality monitoring network for environmental management of port areas An example from the Port of Venice

South Florida Sea Level Rise Projections and Flood Risk Concerns

SPOT4 (Take5) Contribution of Sentinel-2 to coast management

Water Resource Engineering Modeling Applications Overview

How To Measure The Flow Rate Of The Sacramento River With An Adfm

Chapter 12 - HYDROLOGICAL MEASUREMENTS

Dr. Arzu OLGUN TUBİTAK Marmara Research Center TURKEY

6-1 Introduction. 1. Storm drain that does not require pressure testing. 2. Lateral that does not require pressure testing.

Stroomatlas sluis van Wintam

What causes Tides? If tidal forces were based only on mass, the Sun should have a tidegenerating

Lecture 4: Streamflow and Stream Gauging


G3-Giornate Giovani GNRAC Quartiere Fieristico di Ferrara, 21 Settembre 2012

21. Channel flow III ( )

Chapter 9. Steady Flow in Open channels

Background Information: The Mamquam River Floodplain Restoration Project

JASPERS Networking Platform

STORM DRAINS CHAPTER 7

Standard Operating Procedures for Flood Preparation and Response

The Dorset Coast Storms 2014 The Impacts, response, communication & building resilience

Detention Ponds. Detention Ponds. Detention Ponds. Detention Ponds. Detention Ponds. Detention Ponds. CIVL 1112 Detention Ponds - Part 1 1/12

Transcription:

School on Wireless Networking for Scientific Applications in Developing Countries TRIESTE Third week 19-24 Feb 2007 MOSE PROJECT AND HYDRO MORFOLOGICAL MONITORING IN THE VENICE LAGOON Giovanni Cecconi Consorzio Venezia Nuova

OUTLINE A: Mose flood barriers: the importance of the project and a brief presentation of the project B. Monitoring the impact of on-going construction works and the inlet on the hydraulic properties: 1. bathymetric evolution of the sandy bottom at the inlets 2. energy loss through the inlets 3. monitoring velocities and tidal flow 4. residual flow and index of river contamination

Marghera Venice

Salt marshes, channels and tidal creeks Fish farms Valle Zappa

Littorals Pellestrina littoral islands Island of Torcello

Is a transitional environment in a state of instability

SYSTEMS OF INTERVENTIONS

Frequency of high tides >= 110 cm

Relative see level rise

SYSTEMS OF INTERVENTIONS

MOBILE BARRIERS AT THE LAGOON INLETS

MOBILE BARRIERS AT THE LAGOON INLETS HOW THE FLOOD GATES WORK DEFENCE AGAINST EXCEPTIONALLY HIGH TIDES: closures of the inlets for tides > 110 cm

25% of the Mose flood barrier is under construction 33% financed

THE PROJECT - LIDO INLET SITUATION AT JUNE 2006

LIDO INLET WORK SITES reinforcement of the south jetty refuge haven new island

THE PROJECT - MALAMOCCO INLET SITUATION AT JUNE 2006

MALAMOCCO INLET WORK SITES navigation lock the breakwater

THE PROJECT - CHIOGGIA INLET SITUATION AT JUNE 2006

CHIOGGIA INLET WORK SITES refuge haven and the locks the breakwater the inlet today

IMPACT OF FIXED STRUCTURES ON TIDAL FLOW -5 cm average storm surge reduction <10% permanent tidal flow reduction We are monitoring the impact on-going construction works measuring: 1. bathymetric evolution of the sandy bottom at the inlets 2. energy loss through the inlets 3. velocities and tidal flow 4. residual flow and index of river contamination We are building up a DATABASE of monitored data for calibration and validation of hydro-morphological models (hybrid models continuously tuned with experimental data)

Inlets evolution inlet cross sections reduction of the inlet cross section tidal flow lagoon basin flow reduction and velocity increase erosion of the sandy bottom at the inlets

BATHYMETRIC EVOLUTION OF THE SANDY BOTTOM AT THE INLETS acoustic multibeam survey for monitoring bathymetric changes Chioggia inlet: 1.building of a break-water 2.dredge of the navigation channel Erosions or fills can be part of the construction works (dredge of a new navigation channel, building of a new reef ) or the result of velocity changes due to the ongoing construction works

BATHYMETRIC EVOLUTION OF THE SANDY BOTTOM AT THE INLETS evolution of Malamocco inlet from 1999 to October 2006 Evoluzione della barra di foce Progressione dello scavo in bocca Rinforzo testata molo nord Scavo generato dalla protezione del relitto delle ceppe Scavo in prossimità del molo delle ceppe

ENERGY LOSS THROUGH THE INLETS 1. Every inlet has different friction coefficient (depending on bottom surface, length of the reefs..) E TOT = E FRICTION + E VORTEX 2. Every inlet has different volumes of vortex and different volumes of moving flow 3. The situation is different at flood and ebb flow

ENERGY LOSS THROUGH THE INLETS E TOT = E FRICTION + E VORTEX

ENERGY LOSS THROUGH THE INLETS E TOT = E FRICTION + E VORTEX

ENERGY LOSS THROUGH THE INLETS CURVE DI CONTROLLO intensity of tidal flow energy loss velocità media sulla sezione in max flusso/riflusso (cm/s) 150 140 130 120 riflusso 110 100 90 80 70 60 50 40 30 20 10 0-20 -30-40 -50-60 -70-80 -90-100 -110-120 -130-140 -150 bocca di LIDO TREPORTI y = 34.5Ln(x) + 4.9 y = -39.6Ln(x) + 16.8 y = -26.2Ln(x) - 6.8 y = 33.4Ln(x) - 1.2 y = 35.7Ln(x) - 7.9-10 0.0 2.0 4.0 6.0 8.0 10.0 12.0 14.0 16.0 18.0 20.0 22.0 24.0 26.0 28.0 30.0 32.0 flusso mese di aprile 2004 mese di aprile 2004 mese di settembre - ottobre 2005 mese di novembre 2006 mese di novembre 2006 mese di settembre - ottobre 2005 de [cm] y = -35.8Ln(x) + 18.3

MONITORING VELOCITIES AND TIDAL FLOW TIDAL GAGES in the lagoon in the see

MONITORING VELOCITIES AND TIDAL FLOW INSTALLATION OF THE ACOUSTIC FLOW METERS

MONITORING VELOCITIES AND TIDAL FLOW Calibration of the acoustic flow meters: -Bathimetric survey -ADCP shape velocity factor Q = k A v -8.5 Q ADCP /A ADCP 1.6 1.5 1.4 1.3 1.2 1.1 1.0 0.9 0.8 0.7 0.6 0.5 0.4 0.3 0.2 0.1 0.0-0.1-0.2-0.3-0.4-0.5-0.6-0.7-0.8-0.9-1.0-1.1-1.2-1.3-1.4-1.5-1.6 MALAMOCCO - tutte le campagne di misura di agosto 2001, febbraio 2002 e luglio 2004 y = 0.9722x R 2 = 0.9925 FLUSSO RIFLUSSO y = 0.9725x R 2 = 0.9951-1.6-1.4-1.2-1.0-0.8-0.6-0.4-0.2 0.0 0.2 0.4 0.6 0.8 1.0 1.2 1.4 1.6 V -8,5 m (ADCP)

MONITORING VELOCITIES AND TIDAL FLOW misure di VELOCITA DI CORRENTE LIVELLI

MONITORING VELOCITIES AND TIDAL FLOW BOCCA DI LIDO

MONITORING VELOCITIES AND TIDAL FLOW BOCCA DI MALAMOCCO

MONITORING VELOCITIES AND TIDAL FLOW BOCCA DI CHIOGGIA

MONITORING VELOCITIES AND TIDAL FLOW BOCCA DI LIDO : experimental installation of a radar tidal gage and waverecorder

RESIDUAL FLOW AND INDEX OF RIVER CONTAMINATION Evidence of ground-water richarge into the lagoon RESIDUAL FLOW as a percentage of the tidal flux ( 5 333 m3/s ) 2.96% - 5.60%= 2.65% 140 m3/s

RESIDUAL FLOW AND INDEX OF RIVER CONTAMINATION First estimation of the grownd-water richarge into the lagoon

RESIDUAL FLOW AND INDEX OF RIVER CONTAMINATION installation of salinity probes MICROCAT CTD at the inlets at different depth

RESIDUAL FLOW AND INDEX OF RIVER CONTAMINATION Tidal flushing at the lagoon inlets: water recirculation at sea Renewal = V(new) Vin Renewal = Sin,mean - Sout,mean Sin,max-Sout,mean Vin = V(old) + V(new) Recirculation = V(old) =1- Renewal Vin

RESIDUAL FLOW AND INDEX OF RIVER CONTAMINATION Tidal flushing at the lagoon inlets: water recirculation at sea data campagna di misura bocca di porto Salinità max in ingresso Salinità minima in riflusso Volume scambiato (m3) Carico di sale in ingresso (t) Carico di sale in uscita (t) Ricambio Ricircolo Efficienza del ricambio rispetto al ricambio ideale in assenza di ricircoli 30-31/10/02 lido 34.68 31.83 128 812 000 4 368 000 4 282 000 0.46 0.54 0.23 06-07/11/02 lido 34.50 31.93 188 424 000 6 387 000 6 140 000 0.68 0.32 0.51 12-13/11/02 malamocco 35.89 34.34 83 926 000 3 007 000 2 931 000 0.94 0.06 0.58 01-02/04/03 malamocco 35.14 34.37 214 305 000 7 489 000 7 378 000 0.73 0.27 0.67 22-23/03/03 chioggia 35.00 33.80 66 857 000 2 269 000 2 334 000 0.21 0.79 0.11 29-30/03/2003 chioggia 35.40 33.90 101 479 000 3 551 000 3 476 000 0.64 0.36 0.49 15-16/07/04 chioggia 35.91 34.90 88 260 000 3 139 000 3 106 000 0.52 0.48 0.37

RESIDUAL FLOW AND INDEX OF RIVER CONTAMINATION

AT LIDO INLET

CONCLUDING REMARKS The Venice storm surge barriers are a good example of artificial device for flood protection without impacting the sensitive hydromorphological system A monitoring system has been set up for controlling the process In order to improve the reability of the survey system a wi-fi sensor communication system will be tested