ライフサイエンスコーパス: nuclide

1 rface-enhanced NMR spectroscopy to the (17)O nuclide.

2 of the short, 68-min half-life of the (68)Ga nuclide.

3 assuming instant decay of unstable daughter nuclides.

4 of the time with conventional gamma-emitting nuclides.

5 nt fractionation of these two uranium-series nuclides.

6 ent with radioactive powering from r-process nuclides.

7 d the method could be extended to some other nuclides.

8 nct peak-to-peak correlation with cosmogenic nuclide (14)C, total solar irradiance (TSI), and sunspot

9 coherent with time series of the cosmogenic nuclides 14C and 10Be as well as North Atlantic drift ic

10 5)Ac to its ultimate alpha-emitting daughter nuclide (213)Bi, generation of monkey anti-HuM195 antibo

11 isotope shift of the emission lines of both nuclides, (234)U and (238)Pu were selectively and direct

12 abundance from the decay of the short-lived nuclide 60Fe (t(1/2) = 1.49 My) and for possible nucleos

13 -azaacetyl [DO3A]) for the positron-emitting nuclide (64)Cu.

14 corporating the long-lived positron-emitting nuclide (89)Zr were developed using 2 different approach

15 s an inexpensive and readily available radio-nuclide, adds clinically significant information in asse

16 acer candidates were radiolabeled with a PET nuclide and tested in vivo in tau-naive baboons to asses

17 maged 5% of the time using positron-emitting nuclides and 77% of the time with conventional gamma-emi

18 tron excess over the heaviest stable silicon nuclide, and has only one neutron fewer than the heavies

19 diation of mixtures of organics, metals, and nuclides, and the search for life in extreme environment

20 potential for significant toxicity as these nuclides are no longer bound to the carrier IgG.

21 63 were successfully radiolabeled with a PET nuclide at high specific activity, radiochemical purity,

22 owever, with natural radioactive-decay-chain nuclides, because chemical disruption to secular equilib

23 Here we show that the cosmic ray-produced nuclides beryllium-10 and aluminum-26 can be used to dat

24 9 is sufficient to produce other short-lived nuclides, calcium-41 and manganese-53, found in meteorit

25 hanges in production rates of the cosmogenic nuclides carbon-14 and beryllium-10 and centennial to mi

26 We use cosmogenic radio-nuclide (CRN) exposure analysis to record the decay of t

27 ent detailed geomorphological and cosmogenic nuclide data from the southern Ellsworth Mountains in th

28 rphological evidence and multiple cosmogenic nuclide data from the southern Ellsworth Mountains to su

29 Nuclide-dependent SPECT/CT calibration factors were dete

30 CPMS) in two- and three-dimensional (2D, 3D) nuclide distribution mapping beyond the laser beam waist

31 (MMPIs) radiolabeled with positron emitting nuclides (e.g., (18)F) represent a suitable tool for the

32 Here we apply cosmogenic nuclide exposure dating to seven inner gorges along ~500

33 ionuclides into the cell nucleus by means of nuclide-filled liposomes (Nuclisome particles), that is,

34 high specific activity make it an attractive nuclide for labeling and molecular imaging.

35 44)Sc/(47)Sc as an excellent matched pair of nuclides for PET imaging and radionuclide therapy.

36 e, which uses multiple quench parameters for nuclide identification, has been tested on both contamin

37 ming and require some prior knowledge of the nuclide identity to permit accurate quantification.

38 n the electronic environment at each yttrium nuclide in the (Y(3)N)(6+) cluster (more than 200 ppm fo

39 abundance and quadrupolar nature, the (17)O nuclide is very rarely used for spectroscopic investigat

40 ives of most commonly used positron-emitting nuclides make them unsuitable for this purpose.

41 nation of apatite helium ages and cosmogenic nuclides measured in multiple sizes of stream sediment.

42 one neutron fewer than the heaviest silicon nuclide observed so far.

43 Unfortunately, the shorter-lived nuclides of radioxenon, (103)Ru, (89)Sr and (35)S will n

44 netic field intensity minimal and cosmogenic nuclide peaks in ice cores and marine sediments.

45 ted 206-year period in records of cosmogenic nuclide production (carbon-14 and beryllium-10) that is

46 targets, especially concerning the residual nuclide production, the physicochemical behavior of the

47 Here we use recently improved cosmogenic-nuclide production-rate calibrations to recalculate the

48 troduction (e.g., (68)Ga isotope) or optimal nuclide properties for PET imaging (slightly favoring th

49 fluctuations that correlate with cosmogenic nuclide proxies of solar variability, with inferred sola

50 suring almost quantitative labeling and high nuclide purity of final (68)Ga-PSMA(HBED), making subseq

51 Compared with conventional PET nuclides, resolution and quantitation were only slightly

52 erved open-system behavior of uranium-series nuclides, substantially improving the resolution of sea-

53 igh-energy electrons (as would be emitted by nuclides such as (32)P, (90)Y, or (188)Re).

54 Earlier dating with cosmogenic nuclides suffered a high degree of uncertainty and has b

55 riments to be performed on a wide variety of nuclides that are important in bioinorganic chemistry, f

56 e approximately 3,000 stable and radioactive nuclides that either occur naturally on Earth or are syn

57 rates are commonly measured using cosmogenic nuclides, there has been no complementary way to quantif

58 novae sources supplying the p- and r-process nuclides to the solar nebula were thus disconnected or o

59 ughter product relative to its parent (234)U nuclide using inductively coupled plasma mass spectromet

60 ns of the mass-to-charge ratio of the target nuclide were admitted into the octopole reaction cell, t

61 The relative amounts of nuclide were then analyzed in viable and necrotic region

62 In 2011, 100 new nuclides were discovered.

63 nd neutrons, occupies a spot on the chart of nuclides, which is bounded by 'drip lines' indicating th

64 edge of the production history of cosmogenic nuclides, which is needed for geological and archaeologi

65 computing, and find that the number of bound nuclides with between 2 and 120 protons is around 7,000.

66 is overestimate (which is most important for nuclides with large "nonpenetrating" emission components

67 facilitate the introduction of a radioactive nuclide without detrimental effects on the pharmacokinet