1) the amount of mineral dissolution
矿物溶蚀量
1.
t is a new method of studying the water-rock reactions by modeling the reactions and calculating the amount of mineral dissolution between groundwater and rock by the means of liner programming.
采用线性规划的方法模似地下水与岩石之间的作用，计算地下水与岩石之间的矿物溶蚀量是水－岩作用研究的一个新方法。
2) corrosional ratio
溶蚀量
1.
Using the method of standard limestone tablets,the authors detected the corrosional ratios and average corrosional rates of four different vegetation types on the basis of the observation of karst dist.
通过野外溶蚀标准试片法,测试得出重庆金佛山岩溶区碧潭泉和水房泉两泉域4种典型植被类型下的5个测试点的雨季绝对溶蚀量和平均面积溶蚀量。
3) increased thickness for corrosion
腐蚀溶量
4) erosional product
溶蚀产物
5) altered mineral
蚀变矿物
1.
Using absorbed value feature of known mineral criterion for reference,utilizing Landsat 7 ETM remote images and features of altered mineral spectrum from USGS,valuable alteration mineralization information are extracted by comparison of spectrum similarity.
利用该区域的Landsat7 ETM遥感影像和标准光谱库中的特征蚀变矿物光谱为基本数据,借鉴已知矿物标准中的吸收谷特征,应用光谱特征匹配技术进行吸收谷谱区间和吸收谷深度对比,通过比较两者的相似性,达到提取蚀度矿物的目的,提取出许多有价值的似蚀变带遥感信息。
2.
Based on the principle of near-infrared spectrum absorption by altered minerals,optimum measurement wavelength ranges for altered minerals were fixed and qualitative and quantitative analysis for altered minerals in rocks by near infrared spectrometer were accomplished with the mathematics and spectrum learning methods.
基于岩石中蚀变矿物对近红外光谱的吸收原理,确定测量蚀变矿物最佳波长范围,采用数学和谱图学习方法对岩石中蚀变矿物进行定性和定量分析。
6) Altered minerals
蚀变矿物
1.
The altered minerals and their assemblages have traditionally been identified by naked eyes in the field or by microscopes indoors.
利用便携式短波红外光谱测量仪(PIMA)在云南普朗斑岩铜矿区开展了短波红外光谱测量工作,通过系统的野外数据采集,获得了研究区蚀变矿物组合及主要蚀变矿物的分布,并建立了普朗斑岩铜矿区蚀变矿物分带模式。
补充资料：孤峰溶蚀平原
孤峰溶蚀平原是指峰林平原进一步发育，峰林不断溶蚀降低，地表夷平，仅有少量山峰存在所形成的平原
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