摘要
本文运用经典的小孔流速模型及其开放系统的流体力学理论论述了动水位观测原理,证明A—B系统是一种机械换能器,其“水位”随时间t的变化直接反映了主井内的应力状态,而其“流量”则是主井内的真正流量。文中还述及改进动水位观测系统的可能性。
This paper discussed the observational principle of dynamic water-level using the hydro-mechanic theory of the classic small-hole flow-rate model and its open system, which proved that the A-B system is a kind of mechanical transducers, the variation of its water-level with time reflected the stress condition in the main well directly, and its 'outflow' is the real flow in the main well. The paper also discussed the possibility of improving the observational system of dynamic water-level.
出处
《地震》
CSCD
北大核心
1993年第2期55-60,共6页
Earthquake
关键词
动水位
小孔流速模型
地震
观测
dynamic water-level
small-hole flow-rate model and its open system
