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Çѱ¹¼öÀÚ¿øÇÐȸ / v.16, no.3, 1983³â, pp.171-179
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( A Study of Carvernous Limestone Aquifer of Jeon Cheon Basin ) |
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| ÀüõÀ¯¿ª¿¡ ºÐÆ÷µÈ ¾Ï¼®Àº Á¦4±â Åõ¼ö¼ºÀÌ ¾çÈ£ÇÑ ÃæÀûÃþÀÌ ºÒÅõ¼ºÀÌ ¼¼¸³¸Å¼ºÃþÀ» ÇǺ¹Çϸç À̵é Á¦»ç±âÃþÀº Á¦»ï±âÀÇ ¿ª¾Ï ¹× À̾ÏÀ» ºÎÁ¤ÇÕÀûÀ¸·Î ÇǺ¹ÇÑ´Ù. Á¦3±âÃþÇϺο¡´Â °í»ý´ë ´ë¼®È¸¾ÏÅë¿¡ ¼ÓÇÏ´Â Åõ¼ö¼ºÀÌ ¸Å¿ì ¾çÈ£ÇÑ ¼®È¸¾Ï·ù°¡ ¹ß´ÞµÇ¾î ÀÖ´Ù. ÀÌµé ¾Ï¼®Áß¿¡¼ ¿ëÇØ°øµ¿À» ´Ù·® Æ÷ÇÔÇÑ Cambro-Ordovician ±âÀÇ ¼®È¸¾Ï·ù´Â ÇǾР¹× ÀÚÀ¯¸é ´ë¼öÃþÀ¸·Î ±× Åõ¼ö·®°è¼ö°¡ 1,853$m^2$/ÀÏÀ̸ç ÀúÀ¯°è¼ö´Â 1.47 $ imes$$10^{-3}$ÀÌ´Ù. ¶ÇÇÑ º» À¯¿ªÇÏ·ùÃæÀûÆò¾ß¿¡ ¼³Ä¡ÇÑ 3°³ ½ÉÁ¤ÀÇ ºñ¾ç¼ö·®Àº 703ton/ÀÏ/M¿´´Ù. º» ¼®È¸¾Ï³»¿¡ ÀúÀ¯µÈ ½ÉÃþÁöÇϼö·®Àº º» À¯¿ª¿¡ 6³â°£ ³»¸®´Â °¿ì·®°ú ¸À¸Ô´Â 1,059 $ imes$ $10^{6}m^2$ÀÌ°í ¾ÈÀüä¼ö·®Àº 1ÀÏ 126,000§©ÀÌ´Ù. ½Éµµ 80~100m À̳»ÀÇ ½ÉÁ¤ 34°øÀ¸·Î ±¸¼ºµÈ Á¤È£¾çÀ» À¯¿ª Áß.ÇÏ·ùÁö¿ª¿¡ ¼³Ä¡ÇÏ¸é »ó±â ¼®È¸¾Ï´ë¼öÃþÀ¸·ÎºÎÅÍ 1ÀÏ 100,000§©ÀÇ ½ÉÃþÁöÇϼö¸¦ ä¼öÇÒ ¼ö ÀÖ´Ù. |
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| In the Jeon Cheon Basin, unconsolidated alluvium and marine clay beds overlying Tertiary conglomerate and impermeable mudstone, and Cambro-Ordovician sedimentary rocks composed of mainly cavernous limestones, and age-unknowned crystalline rocks are occured. Most productive rock is Cambro-Ordovician limestones containing a lot of solution openings and secondary porosities and shows its transmissivity of 1836$m^2$/day and storativity of 1.47 $ imes$ $10^{-3}$. The storage of deep seated groundwater in linestone aquifer is estimated about 1059 $ imes$ $10^6$ metric tons, being equivalent to 6 years total precipitation of the basin. The safe yield of the groundwater to be abstracted from the aquifer is about 126,000 tons/day. To pump at least 100,000 tons/day of groundwater from the said aquifer, a well field comprising 34 deep wells ranging in depth from 80 to 100 meter and penetrating the cavernous limestone aquifer shall be established at middle and down stream area. |
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Çѱ¹¼öÀÚ¿øÇÐȸÁö / v.16, no.3, 1983³â, pp.171-179
Çѱ¹¼öÀÚ¿øÇÐȸ
ISSN : 1738-9488
UCI : G100:I100-KOI(KISTI1.1003/JNL.JAKO198311920090730)
¾ð¾î : Çѱ¹¾î |
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| ³í¹® Á¦°ø : KISTI Çѱ¹°úÇбâ¼úÁ¤º¸¿¬±¸¿ø |
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