CAJ | 학술논문

以汾源矿5＃煤底板施工注浆钻孔资料为基础，分析了汾源矿奥灰原始导高发育情况及其对煤层开采的影响，得出汾源矿奥灰上马家沟组顶面存在9．1～49．25 m的原始导高；5-101首采面部分区域奥灰原始导高可发育至底板破坏带以上，首采工作面回采存在一定的奥灰突水危险，对5-101工作面进行底板隔水层注浆加固及含水层改造可起到防治水作用，并且对发育有奥灰原始导高的矿井防治水工作也有一定的指导意义。
이분원광5＃매저판시공주장찬공자료위기출，분석료분원광오회원시도고발육정황급기대매층개채적영향，득출분원광오회상마가구조정면존재9．1～49．25 m적원시도고；5-101수채면부분구역오회원시도고가발육지저판파배대이상，수채공작면회채존재일정적오회돌수위험，대5-101공작면진행저판격수층주장가고급함수층개조가기도방치수작용，병차대발육유오회원시도고적광정방치수공작야유일정적지도의의。
On the basis of No.5 coal seam floor injection grouting drill hole data in Fenyuan coal mine,analyzes the ordovician limestone initial water level and the influence to coal seam mining.It obtains that at the top of Shang-majiagou group existing 9 .1 ~49 .25 m initial water level.The ordovician limestone karst initial water level can up to floor damage zone of 5 -101 first mining face partial region,so the first mining face has water inrush danger.Floor aquiclude grouting reinforcement and aquifer reform have important effect for water prevention and control,it also has a guiding significance for the mine water prevention and control of that threaten by the ordovician limestone initial wa-ter level.