Reef Coral Tolerance of High Temperatures and Salinities
Reef Coral Tolerance of High Temperatures and Salinities
复制标题
珊瑚礁珊瑚对高温和盐度的耐受性
作者：
D. Kinsman
匈牙利盆地中第三系及更年轻的岩石体积约为16万千米？孔隙率超过10%的多孔性岩石的体积约为20,000公里“。4,000多公里：温度为60-200摄氏度的热水储存在1,000-3,000米深的岩石孔隙中；大部分热水可以通过在各处打孔来开采，从而形成容量为1-3米：/分钟的热水井。当使用到40摄氏度以下时，这种巨大的储热量相当于2-3x10英寸卡，这大约是1963年底世界已知石油热值的50%。按照我的建议，热水现在正被更大规模地开发用于取暖和工业目的，因为地热供暖比任何其他替代方案都更经济。1000-2000米深度的油井将在几十年内每分钟产生1-3米热水(60-100摄氏度)。
The volume of Tertiary and younger rocks in the Hungarian basin is about 160,000 km?. The volume of porous rocks with porosity over 10 per cent is about 20,000 km". More than 4,000 km º hot water of 60–200 C temperature is stored in the pores of the rocks between 1,000 and 3,000 m depth; most of it can be mobilized by putting down boreholes everywhere to create hot water wells with capacities of 1–3 mº/min. This immense quantity of stored heat when used down to 40 C tempera-ture amounts to 2-3 x 10" º cal, which is about 50 per cent of the calorific value of the world known petroleum doposits at the end of 1963.Following my proposition, the hot water is now being exploited on a greater scale for heating and industrial purposes since geothermal heating is more economic than any other alternative. Wells of 1,000-2,000 m depth will produce 1–3 mº hot water (60–100 C) per min for decades.