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The Upper Tisa Valley. Preparatory proposal for Ramsay

The Upper Tisa Valley. Preparatory proposal for Ramsay

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<strong>The</strong> Strâmturi or Frizia dam and reservoir was built 10 km to the north of Baia<br />

Mare, in the catchment of the Lăpuş, on the Frizia Creek between the years 1960 and<br />

1964. <strong>The</strong> catchment above the dam site is 130 km 2 large, to which 82 km 2 must be<br />

added from the catchment of the Runcu Creek, a tributary of the Mara (which belongs<br />

via the Iza to the <strong>Tisa</strong> stream network). <strong>The</strong> reservoir serves three purposes, viz., water<br />

supply to Baia Mare, power generation and the attenuation of flood waves. <strong>The</strong> dam<br />

proper is 150 m long, but on the right hand side the local rock is concrete lined over 48<br />

m length, so that the dam is actually 198.4 m long. <strong>The</strong> greatest height is 51.5 m. At<br />

normal retention level the water surface is 3 km long, 0.5 km wide and 113 ha large.<br />

<strong>The</strong> total storage space is 17.53 million m 3 , or which 0.93 million m 3 are used <strong>for</strong><br />

flood control purposes. In emergency situations up to 300 m 3 /s can be released. <strong>The</strong><br />

rated discharge of the 4.2 MW Kaplan turbine is 14.5 m 3 /s.<br />

Immediately (300 m) downstream of the Strâmturi dam is the 14.5 m high, r.c.<br />

concrete lined Berdu gravity dam, the reservoir behind which has a maximum capacity<br />

of 133 000 m 3 (at normal retention level 120 000 m 3 ). Mountain water of high quality<br />

is supplied from the reservoir to Baia Mare town over a 5.6 km long pipeline.<br />

<strong>The</strong> Someşul Mic hydropower scheme with its 340 million m 3 of reservoir<br />

capacity has the greatest impact on the river regime. <strong>The</strong> normal annual runoff is 407<br />

million m 3 so that theoretically, 84% of the annual runoff could be stored in the<br />

reservoirs.<br />

328<br />

Table 1. <strong>The</strong> main data of the major reservoirs<br />

<strong>The</strong> reservoirs have changed considerable the flow regime of the Someşul Mic,<br />

in that the monthly mean flows during the late summer later winter low water period<br />

increased (4-82%), while the spring high flows decreased by 8 to 66%. <strong>The</strong> change in

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