您要查找的是不是:
- local meteoric water line (LMWL) 大气降水线
- local meteoric water line 地区降水线
- The slope and the constant item in the meteoric water line (MWL), compared to the global MWL, are both smaller in Kunming, and are related to the evaporation enrichment of heavy isotopes as raindrops fall in unsaturated atmosphere. 与全球大气水线相比,昆明站大气水线的斜率和常数项均较小。 这与雨滴在未饱和大气中降落时重同位素的蒸发富集作用有关。
- Meteoric water line 大气降水线
- The main ore fluid was magma water mixed with meteoric water. 成矿流体是以岩浆水为主,混有古大气水的混合流体。
- Water of hydrothermal fluid was derived from meteoric water. 介质水属于下渗大气降水。
- The part of a ship's hull below the water line. 船底在水线下的船身部分。
- The surface of a ship's hull above the water line. 水上舷侧在齐水线以上船体的表面部分
- DO NOT INSTALL IN THE COLD WATER LINE. 不要安装在冷水管道上。
- Ore-forming fluid rooted in the deep crust mixed with meteoric water. 成矿流体来源于地壳深部和后期大气降水的加入。
- The side of a ship above the water line. 水线上的船的舷侧
- Below the water line of a vessel. 在船的吃水线以下
- Land left dry by a permanent recession of the water line. 海埔新生地海水永久地退后露出的干燥的陆地
- If meteoric water does not evaporate or run overland, it may seep directly into the ground. 如果雨水不从陆地蒸发和流走的话,就可能直接渗入地下。
- A gaining of land by the permanent recession of the water line. 产生新生地因海水永久退去而产生陆地
- The boat was pointing and leaning sharply along the water line. 小船迎风航行,船体沿着水位线严重倾斜。
- The ore fluid is the mixture of granitic water (MCW) and phanerozoic meteoric water or the precambrian mixed water by metamorphism-migmatization. 成矿流体为金铜系列花岗岩岩浆水与显生宙大气降水的混合流体;或为与变质-混合岩化作用有关的早前寒武纪混合水.
- Meteoric water, artificial exploitation and percolation for irrigation canals are the main influence factor of dynamic variation of groundwater. 地下水位频繁的升降一是改变了上覆土体的状态和强度,促进土体崩落;
- Meteoric water leaked and dissolved the lower Paleozoic carbonate rock along faults in Paleogene because of differential upwarding of fault-block. 古近纪断块发生差异升降,大气淡水可以沿断裂渗流到下古生界碳酸盐岩中产生溶蚀作用;
- Due to meteoric water on ground surface, the fluid of outcrop sandstones nowadays show acidity, but, the fluid of core sandstones nowadays is alkality. 露头砂岩由于受地表大气水(酸性水)的影响,现今流体呈酸性,而岩芯砂岩现今流体为碱性流体。
