摘要
作者通过一系列室内、室外实验对水沫状态下的灰华沉积进行了大胆的探索，本文正是根据瀑布水沫及洞灾飞溅水沉积，提出了水沫状态下水－气界面面积的变化及环境ＣＯ２、温度的变化等因素决定着石灰华的沉积速度。
Through a series of indoor and outdoor experiments, the authors give researhing about the tufa deposited in spray state, and based on the deposit of waterfall spray and flying drops in caves, that under the spray state, the velocity of tufa deposition is determined by the change of water-gas bouudary interface area and the change of environment CO2 and temperture. etc
出处
《贵州师范大学学报（自然科学版）》
CAS
1996年第3期62-65,共4页
Journal of Guizhou Normal University：Natural Sciences
基金
贵州省科委基金
