More space for the rivers

More space for the rivers
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AardrijkskundeMiddelbare schoolvmbo t, mavo, havo, vwoLeerjaar 2

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More space for the rivers

Slide 1 - Diapositive

Learning outcome
At the end of the lesson you will know what the Room for the Rivers program entails and what measures have been taken to protect the Netherlands against flooding.

Slide 2 - Diapositive

What do you already know about the Room for the Rivers program?

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Slide 5 - Vidéo

Introduction
The Room for the Rivers program is a plan to protect the Netherlands against flooding.

 What are the main causes of flooding in the Netherlands?

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The 5 most important reasons:

1. Storm surges and sea level rise
2. High water in rivers
3. Extreme precipitation
4. Shortage of water storage and land subsidence
5. Failure of flood defenses

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1. Storm surges and sea level rise

The Netherlands is located on the North Sea, making it sensitive to storm surges. During strong northwesterly storms, the sea level can rise quickly and threaten the coastline. The combination of storms and sea level rise due to climate change increases the risk of flooding. The famous flood disaster of 1953, for example, was caused by a heavy storm surge.

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2. High water in rivers

Large rivers such as the Rhine and the Meuse play an important role in water drainage in the Netherlands. After periods of heavy rainfall or meltwater from the mountains in Switzerland and Germany, these rivers can fill up. High water can cause flooding, especially in winter and spring.

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3. Extreme precipitation

Climate change has increased heavy rainfall. When rainfall is too heavy to be absorbed by the land or drainage systems, it can lead to local flooding. This often happens in cities, where there is a lot of paved surface, such as concrete and asphalt, which reduces the ability of rainwater to infiltrate into the ground.

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4. Shortage of water storage and land subsidence


In certain areas, a shortage of water storage can reduce the ability of water to drain, which increases the risk of flooding. In addition, the soil is sinking in large parts of the Netherlands, especially in peat areas and polders, which increases the risk of flooding.

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5. Failure of flood defenses

The Netherlands is highly dependent on dikes, dunes and other flood defenses to keep the water out. If these barriers fail or are damaged, for example by storms or aging, this can lead to flooding. Strict maintenance and reinforcement measures are essential to prevent this.

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History
The Room for the Rivers program was started in 2006 in response to the floods in 1993 and 1995.

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Measurements
The Room for the Rivers program includes various measures, such as floodplain excavations and dike reinforcements.

What are floodplains and how can floodplain excavations help prevent flooding?

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Floodplain excavations
Floodplain excavations ensure that the river has more space at high water.

What are the advantages of more space for the river?

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Floodplains

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Dike reinforcement


Dike reinforcement is also an important measure of the Room for the Rivers program.

What is dike reinforcement and why is this important?

Slide 17 - Diapositive

Dike reinforcement

Dike raising or dike reinforcement —> the Maas
▪️ The problem is often that there are many houses near the dike, dike reinforcement instead of raising it often occurs.

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River widening
River widening is another measure of the Room for the Rivers program.

What is river widening and how can it help prevent flooding?

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Rivier widening

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Results
The Room for the Rivers program has already produced many results.

What are some of the key results?

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Criticism
The Room for the Rivers program has also received criticism.

What could be points of criticism?

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Future

What are the plans for the future of the Room for the Rivers program?

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Conclusion
The Room for the Rivers program is an important plan to protect the Netherlands against flooding.

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Extra info


Meander
River course

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Meander

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Meanderen

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Meander
Inside bend, slow current and sedimentation

Outside bend, fast current and erosion

Erosion: scouring effect of flowing water, wind or ice

Sedimentation: process where the grains are deposited


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River course
Upper
Middle
Lower
Delta
Sediment

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Write this down

Slide 31 - Diapositive

1. The upper reaches: high in the mountains, where the river originates. Due to the large difference in height, the river flows quickly and the erosive force is great.

2. The middle course: the middle part where the river runs through a valley where it has cut itself.

3. The lower reaches: close to the mouth where the river flows through a river plain. The current speed is low and this increases sedimentation.


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