1) 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。
2) 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。
3) 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。
4) dripstone cave
滴水石洞穴<地>
5) Cave dropstones
洞穴滴石
1.
In particular, Cave dropstones stalagmites offered us a kind of distinctive data source as continental paleoclimate archives.
尤其是洞穴滴石石笋为大陆气候替代指标提供了一类独特的数据源。
6) 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。
补充资料：滴水滩瀑布
滴水滩瀑布在黄果树瀑布以西六公里，这里有二条对峙的险峻山岭—关索岭和大坡顶，是一个深达七百 余米的峡谷。
滴水滩瀑布由三个瀑布组成，最上面叫连天瀑布，中间为冲坑瀑布，下面为高潭瀑布，它是集高、大、美、秀著称的瀑布群。
高：瀑布总高316米，其中冲坑瀑布高160米。高潭瀑布高130米。无论总高度或个体高度都是黄果树瀑布群中最高的。
大：瀑布气势雄伟磅礴，最高一层波涌连天，中间数层翻空涌雪，最下一层震荡群山。
美：远远看去它那美丽多变的姿态宛如一位天仙般的白衣女郎，提着雪白的衣裙轻捷地从高岩上奔跑而来；一忽将裙子收拢束紧，妖媚窈窕；一忽儿又将裙子随意撒开，显得落落大方，潇洒自如。
奇：瀑布的形态多有奇特之处，最上一级瀑布顶仅是一个三点五米宽的峡谷岩道，而最下一级瀑布顶宽则有四十五米。由于它是深切于峡谷之中，多处为山崖遮掩，时隐时现，有的地方只闻其声，不见其形，实难窥其全貌，使人愈觉神秘奇妙。
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