Noun
/kɑːrˈnoʊtaɪt/
Carnotite is a radioactive mineral and a significant ore of uranium and vanadium. It is typically found as yellow or green fine-grained aggregates and usually occurs in sedimentary rocks. The frequency of use in English is relatively low, primarily confined to specific scientific, geological, and mining contexts. It is more commonly encountered in written form in academic articles, textbooks, and professional reports rather than in oral conversation.
Исследователи обнаружили месторождения карнотоита в засушливом регионе на юго-западе.
Due to the radioactive properties of carnotite, safety precautions must be strictly adhered to during mining operations.
Из-за радиоактивных свойств карнотоита необходимо строго соблюдать меры безопасности во время добычи.
The mineralogist published a comprehensive study on the distribution of carnotite in sedimentary basins.
Since "carnotite" is a relatively specific term, it does not commonly appear in idiomatic expressions. However, the discussions around it often involve phrases about radioactive materials, mining, and geology.
Когда дело доходит до добычи радиоактивных материалов, мы должны быть осторожны, особенно с такими минералами, как карнотит.
The team needed to drill down further to get to the heart of the carnotite deposits, as initial surveys showed promise.
Команде нужно было бурить глубже, чтобы добраться до сердца месторождений карнотоита, так как предварительные обследования показали обещания.
The discovery of carnotite changed the landscape of uranium mining in the area.
The term "carnotite" is derived from the name of French physicist and engineer Sadi Carnot, who is known for his work in thermodynamics (specifically in relation to heat engines), combined with the suffix "-ite," which is commonly used to denote minerals and rocks.
The detailed understanding of carnotite is significant in fields related to geology, mining, and material science, especially concerning radioactivity and its applications in energy resources.