CAJ | 학술논문

水洞沟水库是宁蒙交界处的一座工业供水水库，从黄河青铜峡—石嘴山河段用抽水泵站通过压力管道引水。利用2011年10月至2013年11月水库泥沙淤积实测资料，将水库运行阶段分为2011—2014年、2015—2019年、2020—2029年，计算了4种运行方案下的淤积量和平均淤积厚度。结果表明：①水库应尽可能避免在结冰期和含沙量较大的时期进水；②尽可能采用间歇式集中进水的方式；③2011—2014年水库宜采用低水位运行，2015—2019年、2020—2029年宜采用高水位运行；④2015—2019年、2020—2029年宜采用的水库运行方案为每月间歇进水2～3次，其中3月比实际用水量多进水300万m3，4—6月每月均比实际用水量多进水100万m3，其他月份进水量与用水量相等。
수동구수고시저몽교계처적일좌공업공수수고，종황하청동협—석취산하단용추수빙참통과압력관도인수。이용2011년10월지2013년11월수고니사어적실측자료，장수고운행계단분위2011—2014년、2015—2019년、2020—2029년，계산료4충운행방안하적어적량화평균어적후도。결과표명：①수고응진가능피면재결빙기화함사량교대적시기진수；②진가능채용간헐식집중진수적방식；③2011—2014년수고의채용저수위운행，2015—2019년、2020—2029년의채용고수위운행；④2015—2019년、2020—2029년의채용적수고운행방안위매월간헐진수2～3차，기중3월비실제용수량다진수300만m3，4—6월매월균비실제용수량다진수100만m3，기타월빈진수량여용수량상등。
Shuidonggou Reservoir is an industrial water supply reservoir located at the junction of Ningxia and Inner Mongolia of China. Water is diverted to the reservoir through pressure pipeline from the pumping station of the Yellow River from Qingtongxia to Shizuishan. The operational time of the reservoir is divided into three stages,i. e. 2011-2014,2015-2019 and 2020-2029 based on the field measurement data from 2011,and the deposited volume and averaged thickness are calculated under four running schemes. The following conclusions can be obtained:1)The reservoir should avoid water injection during ice formation period or flood period as far as possible;2)It should adopt the intermittent and concentrated water injection scheme as far as possible;3)It is suggested to run the reservoir at lower water level from 2011 to 2014,and to run it at higher water level from 2015 to 2019 and from 2020 to 2029;3)It is suitable to inject water into the reservoir 2 or 3 times intermittently each month. It is suggested to inject extra 3 million m3 water more than actual water requirement in March,while from April to June,it is suggested to injection extra 1 million m3 water more than actual water requirement each month,the water injection amount and water requirement amount should be the same in other months.