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SMALL DAMS PETITS BARRAGES

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Fig. 8.1 – Three small dams in cascade along a farm river, in Brazil.<br />

8.3.5 Failure of Slopes in the Reservoir<br />

Some large dams have been subject to severe damage as a consequence of the failure of big<br />

slopes at the border of the reservoir area. There is not much information about this problem<br />

regarding small dams; nevertheless in some specific places such as reservoirs in very<br />

mountainous regions, it is considered important to analyze the possibility of dam failure or<br />

severe damage caused by the failure of a big slope along the reservoir border, and the big<br />

waves caused by it when hitting the dam.<br />

8.3.6 SABOTAGE<br />

This possibility is not usual in all places, but unfortunately it has to be considered in several<br />

countries nowadays. Nevertheless, this item will not be examined in this ICOLD publication.<br />

8.4 <strong>SMALL</strong> DAM RISK MANAGEMENT<br />

Considering the large number of small dams in most of the countries, (approximately<br />

210.000 dams higher than 5 m in Brazil, 80.000 in Japan, 65,000 IN Spain and 18.000 in South<br />

Korea), it would be practically impossible to apply an EAP for all small dams. Therefore, one of<br />

the first tasks is to perform a complete inventory to identify all small dams in the country, and<br />

select those with a high hazard rating.<br />

According to the National Inventory of Dams (NID), there are approximately 79.500 dams<br />

in United States, including about 11.800 dams that have been considered “high hazard” [1],<br />

meaning that their failure will likely result in loss of life and significant downstream property<br />

damage, what means that 15% are dams with a “high hazard” rating. Considering that small<br />

dams are not so well designed, built and operated as larger dams, it is reasonable to infer that<br />

approximately 30% of the small dams have a “high hazard” rating, and they would need an<br />

EAP.<br />

2<br />

The parameter H . V has no particular scientific significance, but it is an adequate<br />

criterion for the potential hazard classification of small dams, based on the French and Brazilian<br />

experience. It should simply be considered as an indicator of potential risk downstream of the<br />

dam, and correlates well with the peak downstream flood wave, in the event of complete<br />

breaching of the dam.<br />

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