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单词 Iodine isotope
释义

Iodine isotope

中文百科

碘的同位素 Isotopes of iodine

(重定向自Iodine isotope)
附图中,在左肾上腺中心的黑暗球体是一个嗜铬细胞瘤,由放射性碘的MIBG辐射成像。两个图像分别为同一个病人的正面照及背面照。
切尔诺贝利核事故之后各种同位素贡献的放射性占全部放射性剂量(空气中)的比例与与时间的关系图。

(I,原子量:126.90447(3))有37种已知同位素,其中只有碘-127是稳定同位素,其他都具有放射性,因此碘是一种单一同位素元素。天然存在的碘元素中含有两种同位素,主要为127I,以及痕量的129I

除了碘-127之外,其余皆为碘的放射性同位素。在碘的放射性同位素中,寿命最长的是碘-129,半衰期长达1570万年,但仍然远低于原生放射性同位素。自然界中存在痕量的碘-129,但基于宇宙射线生成的碘-129也十分微少,甚至不足以影响原子量的测定,这也使碘因此成为单一同位素元素的原因——在自然界中仅能找到一种稳定的同位素。大部分在地球上存在的碘-129几乎都是人为放射性,主要是因为碘-129是早期核试验以及核事故的一个不须要的长寿命产物。

英语百科

Isotopes of iodine 碘的同位素

(重定向自Iodine isotope)
A Pheochromocytoma is seen as a dark sphere in the center of the body (it is in the left adrenal gland). Image is by MIBG scintigraphy, with radiation from radioiodine in the MIBG. Two images are seen of the same patient from front and back. Note the dark image of the thyroid due to unwanted uptake of radioiodine from the medication by the thyroid gland in the neck. Accumulation at the sides of the head is from salivary gland uptake of iodide. Radioactivity is also seen in the bladder.
The portion of the total radiation activity (in air) contributed by each isotope versus time after the Chernobyl disaster, at the site. Note the prominence of radiation from I-131 and Te-132/I-132 for the first week. (Image using data from the OECD report, and the second edition of 'The radiochemical manual'.[1])
Contribution de différents radioisotopes au niveau de radiation dans l'air après l'accident de Tchernobyl. 131I est en orange.

There are 37 known isotopes of iodine (I) from I to I; all undergo radioactive decay except I, which is stable. Iodine is thus a monoisotopic element.

Its longest-lived radioactive isotope, I, has a half-life of 15.7 million years, which is far too short for it to exist as a primordial nuclide. Cosmogenic sources of I produce very tiny quantities of it that are too small to affect atomic weight measurements; iodine is thus also a mononuclidic element—one that is found in nature only as a single nuclide. Most I derived radioactivity on Earth is man-made, an unwanted long-lived byproduct of early nuclear tests and nuclear fission accidents.

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