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°úÇп¡¼­ »ó´çÇÑ Áøº¸°¡ ÀÎÀ§ÀûÀÎ ÇൿÀ¸·ÎºÎÅÍ À¯¹ßµÈ ÁöÁøÀ¸·ÎºÎÅÍ ¹ß»ýÇÒ ¼ö ÀÖ´Â Áö¹Ý Èçµé¸²(ground shaking) °¡´É¼ºÀ» º¸´Ù ´õ Àß ÀÌÇØÇÒ ¼ö ÀÖ°Ô ÇØÁØ´Ù. ÁöÁø È°µ¿(Earthquake activity)Àº ¹Ì±¹ Áß¾Ó ¹× µ¿ºÎ Áö¿ª¿¡¼­ 2009³â ÀÌÈÄ ¶Ñ·ÇÇÏ°Ô Áõ°¡ÇØ¿Ô´Ù. ÀÌ·¯ÇÑ Áõ°¡´Â ±íÀº À¯Á¤À¸·Î ÁÖÀԵǾú´ø ¼ö¾Ð ÆļâÀÇ ¹°¿¡¼­ ¹ß»ýÇÏ´Â Æó¼ö¸¦ Æó±âÇÏ´Â »ê¾÷Àû ¿î¿µ°ú °ü·ÃÀÌ ÀÖ´Ù.

¹Ì±¹ ÁöÁú ¿¬±¸¼Ò(USGS; U. S. Geological Survey)´Â ÁöÁø È°µ¿µµ(seismicity)°¡ ¶Ñ·ÇÇÏ°Ô Áõ°¡ÇÑ °ÍÀ¸·Î ±â·ÏµÈ Áö¿ª¿¡¼­ À§ÇèÇÑ Áö¹Ý Èçµé¸²ÀÌ ¾î¶»°Ô ±â·ÏµÉ ¼ö Àִ°¡¸¦ ¿¹ÃøÇϱâ À§ÇÑ ¿¹ºñ ¸ðµ¨ÀÇ À±°ûÀ» ¼³¸íÇÏ´Â º¸°í¼­¸¦ 2015³â 4¿ù 27ÀÏ ¹ßÇ¥Çß´Ù. ¸ðµ¨Àº ±Ã±ØÀûÀ¸·Î ¾ó¸¶³ª ºó¹øÇÏ°Ô ÁöÁøÀÌ ³»³â¿¡ ¹ß»ýÇÒ °ÍÀÎÁö¸¦ °è»êÇÏ°í, ±× °á°ú·Î ´Ü´ÜÇÑ Áö¹ÝÀÌ ¾î¶»°Ô Èçµé¸± °ÍÀΰ¡¸¦ °è»êÇÏ´Â °ÍÀ» ¸ñÇ¥·Î ÇÏ°í ÀÖ´Ù. ÀÌ º¸°í¼­´Â Áß¾Ó ¹× µ¿ºÎ ¹Ì±¹ Áö¿ªÀ» Á¶»çÇß´Ù. ¹Ì·¡ ¿¬±¸´Â ¼­ºÎ Áö¿ª ÁַκÎÅÍ ¾òÀº ÀÚ·á¿Í ÅëÇÕµÉ °ÍÀÌ´Ù.

¶Ç ÀÌ º¸°í¼­´Â ¿¹ºñ ¸ðµ¨¿¡ ´ëÇÑ Ãß°¡ÀûÀÎ Á¶»ç¸¦ °ÅÃÄ 2015³â ¸» ¹ßÇ¥µÉ °ÍÀ¸·Î °èȹµÈ ÃÖÁ¾ÀûÀÎ À§Çè ¸ðµ¨(hazard model)À» °³¹ßÇϱâ À§ÇÏ¿© ÇØ°áµÉ ÇÊ¿ä°¡ ÀÖ´Â ¹®Á¦¸¦ ±Ô¸íÇß´Ù. ÀÌ·¯ÇÑ ¿¹ºñ ¸ðµ¨Àº Çö½ÇÀûÀ¸·Î ½ÇÇèÀ¸·Î °£ÁֵǾî¾ß¸¸ ÇÏ°í, ÀÇ»ç °áÁ¤¿¡ »ç¿ëµÇ¾î¼­´Â ¾È µÈ´Ù.

USGS °úÇÐÀÚµéÀº À¯¹ßµÈ ÁöÁø È°µ¿µµÀÇ Áõ°¡µÈ ºñÀ²À» ³ªÅ¸³»´Â 8°³ ÁÖ ³»¿¡¼­ 17°³ Áö¿ªÀ» ±Ô¸íÇß´Ù. 2000³â ÀÌÈÄ ÀÌ·¯ÇÑ Áö¿ªÀÇ ¸î¸î °÷Àº 2009³â ÀÌÈÄ »ó´çÈ÷ Áõ°¡ÇßÀ¸¸ç ¿À´Ã³¯±îÁö À̾îÁö°í ÀÖ´Â ³ôÀº ¼öÁØÀÇ ÁöÁø È°µ¿µµ¸¦ °æÇèÇÏ°í ÀÖ´Ù. ÀÌ ¿¬±¸´Â ÀÌ·¯ÇÑ Áö¿ª¿¡¼­ À¯¹ßµÈ ÁöÁø°ú »ó°ü°ü°è¸¦ ¸Î°í ÀÖ´Â À§ÇèÇÑ ¼öÁØ¿¡ ´ëÇÑ Ã¹ ¹ø° Æ÷°ýÀûÀÎ Æò°¡ÀÌ´Ù. ÀÌ Áö¿ªÀÇ ¼¼ºÎÀûÀÎ ¸®½ºÆ®´Â ÇÔ²² °ÔÀçµÈ Áöµµ¿¡ Á¦°øµÇ°í ÀÖÀ¸¸ç, ¾Ù¶ó¹è¸¶ ÁÖ, ¾ÆÄ­¼Ò ÁÖ, ÄÝ·Î¶óµµ ÁÖ, ĵÀÚ½º ÁÖ, ´º¸ß½ÃÄÚ ÁÖ, ¿ÀÇÏÀÌ¿À ÁÖ, ¿ÀŬ¶óÈ£¸¶ ÁÖ ¹× Åػ罺 ÁÖ µîÀÌ Æ÷ÇԵȴÙ.

°úÇÐÀÚµéÀº ÀÌ·¯ÇÑ Áö¿ª¿¡¼­ ÁöÁøÀ» ºÐ¼®ÇÏ°í, ÁöÁøÀÇ ºñÀ², À§Ä¡, ÃÖ´ë Å©±â ¹× Áöµ¿(ground motion) µîÀ» °í·ÁÇÔÀ¸·Î½á ¸ðµ¨À» °³¹ßÇß´Ù.

ÀÌ·¯ÇÑ »õ·Î¿î º¸°í¼­´Â ÁÖÀÔ À¯¹ß ÁöÁø(injection-induced earthquakes)ÀÌ ¾î¶»°Ô ¹Ì±¹ ÁöÁø À§Çè Áöµµ(seismic hazard map)¿¡ ÅëÇÕµÉ ¼ö ÀÖ´ÂÁö¸¦ ±â¼úÇÑ Ã¹ »ç·Ê¶ó°í USGS »êÇÏ ±¹¸³ ÁöÁø À§Çè ¸ðµ¨¸µ ÇÁ·ÎÁ§Æ® Ã¥ÀÓÀÚÀÎ Mark PetersenÀº ¹àÇû´Ù. ÀÌ·¯ÇÑ ÁöÁøÀÌ ÀÌÀüº¸´Ù ´õ ³ôÀº ºñÀ²·Î ¹ß»ýÇÏ°í ÀÖÀ¸¸ç, Àαٿ¡ °ÅÁÖÇÏ´Â »ç¶÷µéÀÌ ÈξÀ ´õ ³ôÀº À§Çè¿¡ ³ëÃâµÇ°í ÀÖ´Ù°í PetersenÀº ÁöÀûÇß´Ù. USGS´Â Áö¹Ý Èçµé¸²À¸·ÎºÎÅÍ Áö¿ª »çȸ¸¦ ¾ÈÀüÇÏ°Ô À¯ÁöÇÏ´Â µ¥ µµ¿òÀ» ÁÖ´Â °áÁ¤À» Áö¿øÇϱâ À§ÇÏ¿© ÀÌ·¯ÇÑ Áö¿ª¿¡¼­ ÁöÁø À§Ç輺(seismic hazards)À» Æò°¡Çϴµ¥ °É¸²µ¹ÀÌ µÇ°í ÀÖ´Â ¹®Á¦¸¦ ±Øº¹ÇÏ´Â ¹æ¾ÈÀ» °³¹ß ÁßÀ̶ó°í PetersenÀº µ¡ºÙ¿´´Ù.

2014³â USGS´Â ÀÚ¿¬ÀûÀÎ ÁöÁø¿¡ ´ëÇÏ¿© À§ÇèÇÑ ¼öÁØÀ» ±â¼úÇØÁÖ´Â ÃֽŠ±¹°¡ ÁöÁø À§Çè Áöµµ(National Seismic Hazard Maps)¸¦ ¹ßÇ¥Çß´Ù. ÀÌ·¯ÇÑ Áöµµ´Â µµ½Ã °ÇÃà¹ý ±ÔÁ¤(building codes), º¸Çè·ü(insurance rates), ºñ»ó ´ëÃ¥ °èȹ(emergency preparedness plans) ¹× ´Ù¸¥ Àû¿ë µîÀ» »ç¿ëÇß´Ù. ÀÌ·¯ÇÑ Áöµµ´Â °Ç¹°ÀÇ Æò±Õ ¼ö¸íÀÎ 50³âÀÇ ±â°£ À̳»¿¡ ÁöÁø Èçµé¸²ÀÇ °¡´É¼ºÀ» ¿¹ÃøÇß´Ù. ±×·¯³ª ÀÌ·¯ÇÑ »õ·Ó°Ô À¯¹ßµÈ ÁöÁø È°µ¿µµ »ý¼º¹°Àº 1³âÀÇ ±â°£ ³»¿¡ À¯¹ßµÈ ÁöÁøÀ¸·ÎºÎÅÍ °¡´ÉÇÑ Áö¹Ý Èçµé¸²ÀÇ °­µµ¸¦ º¸¿©ÁØ´Ù. ÀÌ·¯ÇÑ ´õ ªÀº ±â°£Àº ÀûÀýÇÏ´Ù. ¾î´À ÁöÁ¡¿¡¼­ º¯È­µÉ ¼ö ÀÖ´Â »ó¾÷ÀûÀÎ °áÁ¤°ú Á¤Ã¥Àû °áÁ¤¿¡ Á¿ìµÉ ¼ö Àֱ⠶§¹®¿¡, À¯¹ßµÈ È°µ¿ÀÌ ½Ã°£¿¡ µû¶ó ±Þ°ÝÇÏ°Ô ´Þ¶óÁú ¼ö ÀÖ´Ù.

ÀÌ·¯ÇÑ »õ·Î¿î ¹æ¹ý°ú »ý¼º¹°Àº USGS¿Í ¿ÀŬ¶óÈ£¸¶ ÁöÁú Á¶»ç(Oklahoma Geological Survey)°¡ ÁÖ°üÇÑ ¿öÅ©¼óÀÇ ÀÏȯÀ¸·Î ¾ò¾îÁ³´Ù. ÀÌ º¸°í¼­¿¡¼­ ±â¼úµÈ ¿öÅ©¼óÀº À¯¹ßµÈ ÁöÁøÀ¸·ÎºÎÅÍ À§ÇèÀ» ³íÀÇÇϱâ À§ÇÑ Á¤ºÎ, »ê¾÷ ¹× ÇÐ°è °ü°èÀÚ µîÀÇ Æø³ÐÀº Àü¹®°¡ Áý´ÜÀÌ Âü¿©Çß´Ù.

È­Çй°Áú¿¡ ÀÇÇÏ¿© ¿À¿° ¶Ç´Â ¿°ºÐÀ» ÇÔÀ¯ÇÑ Æó¼ö(wastewater)´Â ´ã¼ö °ø±Þ¿ø¿¡ ´ëÇÑ ¿À¿°À» ¿¹¹æÇÒ ¼ö ÀÖ´Â ¹æ½ÄÀ¸·Î Æó±âµÉ ÇÊ¿ä°¡ ÀÖ´Ù. ´Ù·®ÀÇ Æó¼ö´Â ¿¡³ÊÁö »ý»êÀ¸·ÎºÎÅÍ ºÎ»ê¹°°ú °°Àº ´Ù¾çÇÑ °øÁ¤ÀÇ °á°ú·Î »ý¼ºµÉ ¼ö ÀÖ´Ù. Æó¼ö ÁÖÀÔÀº ÁöÇÏÀÇ °ø±Ø ³» ¾Ð·Â(pore pressure)À» Áõ°¡½ÃŲ´Ù. ÀÌ·¯ÇÑ °ø±ØÀÇ ¾Ð·Â Áõ°¡´Â ÁöÁøÀ» ´õ ¸¹ÀÌ ¹ß»ý½ÃÅ°´Â ¿øÀÎÀÌ µÇ´Â Àα٠´ÜÃþÀ» ¸Å²ô·´°Ô ÇÑ´Ù. ºñ·Ï Æó±â °øÁ¤ÀÌ ÁöÁøÀ» Ã˹ßÇÒ ¼ö ÀÖ´Â °¡´É¼ºÀÌ ÀÖ´Ù°í ÇÏ´õ¶óµµ, ´ëºÎºÐÀÇ Æó¼ö Æó±â À¯Á¤Àº À¯°¨ ÁöÁø(felt earthquakes)À» »ý¼º½ÃÅ°Áö ¾Ê´Â´Ù.

¸¹Àº Àǹ®ÀÌ ¼ö¾Ð Æļâ(hydraulic fracturing, ÀϹÝÀûÀ¸·Î Æļâ¶ó°í ¾ð±ÞµÇ°í ÀÖÀ½)°¡ ÃÖ±Ù ÁöÁøÀÇ Áõ°¡¿¡ Ã¥ÀÓÀÌ ÀÖ´ÂÁö ¿©ºÎ¿¡ ´ëÇÏ¿© Á¦±âµÆ´Ù. USGSÀÇ ¿¬±¸´Â ½ÇÁ¦ÀûÀÎ ¼ö¾Ð Æļ⠰øÁ¤ÀÌ À¯ÀÏÇÑ À¯°¨ ÁöÁøÀÇ Á÷Á¢ÀûÀÎ ¿øÀÎÀ̶ó°í Á¦¾ÈÇß´Ù.

½ÇÁ¦ »õ·Ó°Ô ¹ßÇ¥µÈ USGS º¸°í¼­´Â ¡°2014³â ¹Ì±¹ ±¹°¡ ÁöÁø À§Çè ¸ðµ¨¿¡¼­ À¯¹ß ÁöÁø È°µ¿µµÀÇ ÅëÇÕ-2014³â ¿öÅ©¼ó°ú ÁöÁø È°µ¿µµ ¿¬±¸ÀÇ °á°ú(Incorporating Induced Seismicity in the 2014 United States National Seismic Hazard Model—Results of 2014 Workshop and Sensitivity Studies.)¡±ÀÌ´Ù.

±×¸²1> À¯¹ß ÁöÁø È°µ¿ÀÇ Áõ°¡µÈ ºñÀ²À» °¡Áø ¹Ì±¹ ÁßºÎ¿Í µ¿ºÎ Áö¿ª¿¡ 17°³ Áö¿ªÀ» ±Ô¸íÇÑ »õ·Î¿î ¿¬±¸.
 
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Fracking? Injecting wastewater? New insight on ground shaking from human-made earthquakes

Significant strides in science have been made to better understand potential ground shaking from induced earthquakes, which are earthquakes triggered by human practices.

Earthquake activity has sharply increased since 2009 in the central and eastern United States. The increase has been linked to industrial operations that dispose of wastewater by injecting it into deep wells.

The U. S. Geological Survey (USGS) released a report today that outlines a preliminary set of models to forecast how hazardous ground shaking could be in the areas where sharp increases in seismicity have been recorded. The models ultimately aim to calculate how often earthquakes are expected to occur in the next year and how hard the ground will likely shake as a result. This report looked at the central and eastern United States; future research will incorporate data from the western states as well.

This report also identifies issues that must be resolved to develop a final hazard model, which is scheduled for release at the end of the year after the preliminary models are further examined. These preliminary models should be considered experimental in nature and should not be used for decision-making.

USGS scientists identified 17 areas within eight states with increased rates of induced seismicity. Since 2000, several of these areas have experienced high levels of seismicity, with substantial increases since 2009 that continue today. This is the first comprehensive assessment of the hazard levels associated with induced earthquakes in these areas. A detailed list of these areas is provided in the accompanying map, including the states of Alabama, Arkansas, Colorado, Kansas, New Mexico, Ohio, Oklahoma, and Texas.

Scientists developed the models by analyzing earthquakes in these zones and considering their rates, locations, maximum magnitude, and ground motions.

"This new report describes for the first time how injection-induced earthquakes can be incorporated into U.S. seismic hazard maps," said Mark Petersen, Chief of the USGS National Seismic Hazard Modeling Project. "These earthquakes are occurring at a higher rate than ever before and pose a much greater risk to people living nearby. The USGS is developing methods that overcome the challenges in assessing seismic hazards in these regions in order to support decisions that help keep communities safe from ground shaking."

In 2014, the USGS released updated National Seismic Hazard Maps, which describe hazard levels for natural earthquakes. Those maps are used in building codes, insurance rates, emergency preparedness plans, and other applications. The maps forecast the likelihood of earthquake shaking within a 50-year period, which is the average lifetime of a building. However, these new induced seismicity products display intensity of potential ground shaking from induced earthquakes in a one-year period. This shorter timeframe is appropriate because the induced activity can vary rapidly with time and is subject to commercial and policy decisions that could change at any point.

These new methods and products result in part from a workshop hosted by the USGS and the Oklahoma Geological Survey. The workshop, described in the new report, brought together a broad group of experts from government, industry and academic communities to discuss the hazards from induced earthquakes.

Wastewater that is salty or polluted by chemicals needs to be disposed of in a manner that prevents contaminating freshwater sources. Large volumes of wastewater can result from a variety of processes, such as a byproduct from energy production. Wastewater injection increases the underground pore pressure, which may lubricate nearby faults thereby making earthquakes more likely to occur. Although the disposal process has the potential to trigger earthquakes, most wastewater disposal wells do not produce felt earthquakes.

Many questions have been raised about whether hydraulic fracturing -- commonly referred to as "fracking" -- is responsible for the recent increase of earthquakes. USGS's studies suggest that the actual hydraulic fracturing process is only occasionally the direct cause of felt earthquakes.

Real the newly published USGS report, ¡°Incorporating Induced Seismicity in the 2014 United States National Seismic Hazard Model—Results of 2014 Workshop and Sensitivity Studies.¡±
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