1) tunnel flow
洞穴水流
1.
Based on detailed monitoring of tunnel systems, it was found that tunnel flow hydrological processes were characterized by a quick response to rainfall, an early flow peak, and a short duration.
通过对黄土高原丘陵沟壑区典型小流域洞穴系统应用烟幕弹进行调查和实际观测揭示了黄土洞穴系统水流的水文特性：产流初始时间、水流峰值特性、水流历时，以及黄土洞穴系统的不稳定对洞穴水流不文特性的影响等。
2) 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。
3) 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。
4) 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。
5) cave water
洞穴水系
1.
Implication for sampling paleo-climate indicators by monitoring seasonal variations of δD and δ~(18)O in cave waters;
洞穴水系氢氧同位素监测对重建古气候样品选择的指示意义
6) inflow cave
流入型洞穴
1.
As a typical inflow cave,Jiutiandong is formed by direct recharge of allogenic water.
九天洞是一个典型的直接由外源水补给形成的流入型洞穴。
补充资料：阿尔塔米拉洞穴壁画
| 阿尔塔米拉洞穴壁画 rock paintings of Altamira Cave 欧洲旧石器时代晚期壁画。在西班牙北部桑坦德市的阿尔塔米拉洞穴内。1879年发现。最初学术界不同意是原始人的作品，至 1902 年才获承认。洞穴长270米，大部分壁画分布在长18米的侧洞的顶和壁上。内容主要是涂有红、黑、紫色的成群野牛，还有野猪、野马和赤鹿等，总数达150多只。这些动物形象描画得细腻生动，栩栩如生。其中画一头野牛受伤卧地，低头怒视前方，把牛的野性表现得十分逼真，被公认为世界美术史上原始绘画的代表作。洞中还有镌刻的人物形象及手轮廓图形等。在洞穴前部，发现了旧石器时代晚期文化的遗物，为确定岩画的年代提供了证据。一般认为，壁画内容可能与原始人祈求狩猎成功的巫术活动有关。
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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