नियोडाइमियम हिंदी उपयोग और उदाहरण

इसको बनाने में लेजर पदार्थ नियोडाइमियम को याट्रियम एल्यूमिनियम गारनेट में डोप किया गया था।

लैन्थनाइड नियोडाइमियम (Neodymium) एक रासायनिक तत्व है जिसका प्रतीक Nd है।

आधुनिक ड्राइवर चुंबक लगभग हमेशा स्थायी होते हैं और चीनी मिट्टी, फेराइट, एल्किनो या अधिक हाल में, दुर्लभ मृदा जैसे नियोडाइमियम और सैमेरियम कोबाल्ट के बने होते हैं।

| 60 || नियोडाइमियम || Nd || Neodymium।

|नियोडाइमियम||Neodymium||Nd||60||144.242(3)||'nbsp;||6।

""लैन्थनाइड नियोडाइमियम (Neodymium) एक रासायनिक तत्व है जिसका प्रतीक Nd है।

नियोडाइमियम इसके अंग्रेजी अर्थ का उदाहरण

Sept 2007 : SDK opened its second neodymium-based alloys plant in China.

Parisite is mostly parisite-(Ce), but when neodymium is present in the structure the mineral becomes parisite-(Nd).

Bastnasite is a cerium lanthanum and neodymium fluoro-carbonate (CeF)CO3, from Bastnas, near Riddarhyttan, in Vestmanland, Sweden, and the Pikes Peak region in Colorado, United States.

Generally, the active medium of a solid-state laser consists of a glass or crystalline "host" material, to which is added a "dopant" such as neodymium, chromium, erbium, thulium or ytterbium.

Of these, probably the most common is neodymium-doped yttrium aluminum garnet (Nd:YAG).

Nd:YAG – neodymium-doped yttrium aluminium garnet, Nd:Y3Al5O12.

Nd:YCOB – neodymium-doped YCOB, YCa4O(BO3)3.

Each neodymium ion replaces a yttrium ion in the YCOB crystal structure.

Polycrystalline Mn:SrAl12O19 is used as a green phosphor for plasma displays, and when doped with praseodymium or neodymium it can act as a good active laser medium.

Production economics Samarium–neodymium dating is a radiometric dating method useful for determining the ages of rocks and meteorites, based on the radioactive decay of a long-lived samarium isotope (147Sm) to a radiogenic neodymium isotope (143Nd).

Neodymium isotope ratios together with samarium-neodymium ratios are used to provide information on age information and the source of igneous melts.

It is sometimes assumed that at the moment when crustal material is formed from the mantle the neodymium isotope ratio depends only on the time when this event occurred, but thereafter it evolves in a way that depends on the new ratio of samarium to neodymium in the crustal material, which will be different from the ratio in the mantle material.

Samarium–neodymium dating allows us to determine when the crustal material was formed.

Samarium has five naturally occurring isotopes, and neodymium has seven.