Jökull


Jökull - 01.12.1961, Blaðsíða 54

Jökull - 01.12.1961, Blaðsíða 54
er above 100° C is preventecl from flashing and, also, that the boreholes can be pumped according to demand, at least to a certain degree. During periods of heavy demand the pumping exceeds the free flow of the holes. On the other hand, the flow is below the free flow during periods of low demand. In this manner the storing capacity of the thermal area is utilized which is of great economic importance. In fact, as will be dis- cussed below, this appears to be the most ef- ficient method of loadregulation. This methocl is, however, relatively new in Iceland ancl has to be tested in the long run. At this juncture it appears aclvisable to limit the pumping of the boreholes to a certain ratio of the annual free flow. Over-pumping may lead to an infiltration of cold water. 4. MAIN SUPPLY PIPE-LINES. The great thermal areas in Krýsuvik and Hengill which are located 30 km south re- spectively 45 km east of Reykjavik are poten- tial sources of natural steam at pressures up to 15 atm abs and high-temperature water up to a temperature of 200° C, or possibly more. The exploitation of these areas for heating in the Reykjavik area involves the piping of low-press- ure steam or high-temperature water over con- siclerable distances. The question arises as to the most efficient and economical piping system. Three factors are of basic importance. First, domestic heating constitutes the main market in the Reykjavik area. Hot water is therefore to be preferred as the medium distributed to the consumers in the city. Second, the boreholes produce wet steam with a water/steam ratio be- tween 4 and 6. There are consequently large quantities of liigh-temperature water available. Third, the specific volume of low-pressure steam is very unfavourable ancl implies large cross- sections of the pipelines. These factors iniply that hight-temperature water is much to be preferred as the medium for piping over distances more than a few kilo- meters. Water temperature in the range 160 to 180° C or possibly up to 200° C are to be app- lied. Heated surface water is to be preferred to the thermal water due to the chemical im- purities in the latter. 5. DISTRIBUTION SYSTEMS. (a) Type of clistribution system. Practically all houses in Iceland have central heating systems. The systems in the smaller houses burn gas-oil whereas the larger houses use a lower grade of fuel oil. The central systems are generally designed for a maximum riser temperature of 60 to 80° C. This design temp- erature is, however, considerably above the real maximum occurring af ordinary conditions. On the other hand, thermal water is available from some of the thermal areas at temperatures considerably above the maximum riser tempera- ture. This high-temperature water can be used for domestic lieating in ordinary system in two ways. Firstly, by means of two-pipe circulating systems connected to the house systems either directly, or indirectly through heat-exchangers. The temperature of the outgoing water is controlled by the the rate of circulation and is kept at a maximum of 90° C. Secondly, by nteans of one-pipe distribution systems connected indi- rectly through heat exchangers to the house- systems. The temperature in the riser is then controllecl by automatic equipment which opera- tes on the intake flow. The application of lieat-exchangers has the advantage that the house-systems are not ex- posecl to the thermal water. Some thermal waters are corrosive and form scale in pipes and radi- ators. Tliis is rather serious mainly in the case of the house-systems as the pipes are generally built into the walls of the houses. Moreover, the heat-excliangers may be necessary because of pressure conditions. On the other hand, the heat-exchangers re- present additional investment and the efficiency of the system may be slightly affected. In a single- pipe system the temperature drop through the exchanger is lost ancl this may reduce the over- all system efficiency by as much as 5 to 10%. In a two-pipe system, on the other liand, the heat-exchangers do not induce losses to the system if the effluent hot-water is applicable in other heating systems. The tap-water supply is of some importance. The distribution of water with temperatures above 100° C may make special heat-exchang- ers either for the heating of tap-water or the cooling of thermal water to tap-water tempera- 52
Blaðsíða 1
Blaðsíða 2
Blaðsíða 3
Blaðsíða 4
Blaðsíða 5
Blaðsíða 6
Blaðsíða 7
Blaðsíða 8
Blaðsíða 9
Blaðsíða 10
Blaðsíða 11
Blaðsíða 12
Blaðsíða 13
Blaðsíða 14
Blaðsíða 15
Blaðsíða 16
Blaðsíða 17
Blaðsíða 18
Blaðsíða 19
Blaðsíða 20
Blaðsíða 21
Blaðsíða 22
Blaðsíða 23
Blaðsíða 24
Blaðsíða 25
Blaðsíða 26
Blaðsíða 27
Blaðsíða 28
Blaðsíða 29
Blaðsíða 30
Blaðsíða 31
Blaðsíða 32
Blaðsíða 33
Blaðsíða 34
Blaðsíða 35
Blaðsíða 36
Blaðsíða 37
Blaðsíða 38
Blaðsíða 39
Blaðsíða 40
Blaðsíða 41
Blaðsíða 42
Blaðsíða 43
Blaðsíða 44
Blaðsíða 45
Blaðsíða 46
Blaðsíða 47
Blaðsíða 48
Blaðsíða 49
Blaðsíða 50
Blaðsíða 51
Blaðsíða 52
Blaðsíða 53
Blaðsíða 54
Blaðsíða 55
Blaðsíða 56
Blaðsíða 57
Blaðsíða 58
Blaðsíða 59
Blaðsíða 60
Blaðsíða 61
Blaðsíða 62
Blaðsíða 63
Blaðsíða 64
Blaðsíða 65
Blaðsíða 66
Blaðsíða 67
Blaðsíða 68

x

Jökull

Beinir tenglar

Ef þú vilt tengja á þennan titil, vinsamlegast notaðu þessa tengla:

Tengja á þennan titil: Jökull
https://timarit.is/publication/1155

Tengja á þetta tölublað:

Tengja á þessa síðu:

Tengja á þessa grein:

Vinsamlegast ekki tengja beint á myndir eða PDF skjöl á Tímarit.is þar sem slíkar slóðir geta breyst án fyrirvara. Notið slóðirnar hér fyrir ofan til að tengja á vefinn.