1) ancient cave watey zone
古洞穴水带
2) paleocave
古洞穴
1.
For the sake of building a realistic geological model of the paleocave carbonate reservoir, correlation has been made with the paleocaves occurred in Wudaoban outcrop sections in Bachu area.
古洞穴型碳酸盐岩储层都具有显著的非均质性和预测难度大的特点。
3) cave archeology
洞穴考古
4) cave drip water
洞穴滴水
1.
An understanding of temporal and spatial variability of cave drip water geochemistry is thus important in studying the stalagmite records for interpreting the paleoclimatic change.
本文选取重庆武隆芙蓉洞作为对象，从水文水化学方面分析芙蓉洞洞穴滴水的水文学和元素地球化学特征，监测指标包含了洞穴滴水中的滴水滴率、电导、pH、水温、Ca~(2+)、Mg~(2+)、K~+、Na~+、Sr~(2+)、Ba~(2+)、SO_4~(2-)、HCO_3~-、Cl~-、，同时对洞穴环境指标如温度等以及洞顶上方泉水的Ca~(2+)、Mg~(2+)、K~+、Na~+、Sr~(2+)、Ba~(2+)、SO_4~(2-)、HCO_3~-、Cl~-等也进行了长期的动态监测。
5) drip water
洞穴滴水
1.
Temporal-spatial variation of SO_4~(2-) concentration of the drip water and its significance in the Shihua cave,Beijing
北京石花洞洞穴滴水中硫酸根浓度的时空变化及其意义
2.
Our monitoring for drip water through a hydrologic year in Panlong cave of Guilin indicates that cave drip water is of quick response to atmospheric precipitation and the recorded features by the drip water can directly reflect the physical and chemical characteristics of atmospheric precipitation.
洞穴滴水主要来源于大气降水的入渗,是岩溶洞穴内的低能量的渗流水,它受控于水-土-岩的相互作用。
3.
According to the research of element geochemistry,water transporting in the cave roof influenced the sources of the substances,and the substances in drip water mainly come from the soil and rock in the roof of Qixing cave and the fewer content of elements origins from the rainfall.
洞穴滴水的化学组成中元素含量变化主要由水运移过程中水-土、水-岩作用导致的岩石溶解-方解石沉淀过程所控制。
6) cave dripping water
洞穴滴水
1.
Cave dripping water datalogger is special designed for recording the parameters of cave dripping water,which will possibly provide fundamental information to well understand the climatic significance of annual layer of stalagmite.
洞穴水滴记录仪是为研究石笋年层气候意义而专门设计的记录洞穴滴水速率参数的仪器。
补充资料：经水带黄混浊
经水带黄混浊
病名。见清·沈尧封《女科辑要·卷上》。指月经色黄夹杂混浊液体者。多由脾虚失运，湿痰下注所致。《女科辑要》引李氏：“经水带黄混浊者，湿痰也。”治宜健脾益气，除湿化痰。方选二陈汤加减。
说明：补充资料仅用于学习参考，请勿用于其它任何用途。
参考词条