ライフサイエンスコーパス: iron isotope

コーパス検索結果 (１語後でソート)

通し番号をクリックするとPubMedの該当ページを表示します

1 th oral (57Fe) and intravenous (58Fe) stable iron isotopes.

2 ted from erythrocyte incorporation of stable iron isotopes 14 d after administration.

3 irect on-line detection of the most abundant iron isotope 56Fe without interference from 40Ar16O.

4 stered on days 1 and 15 contained the stable iron isotopes (57)Fe and (58)Fe, respectively, and eryth

5 We report the first iron isotope analysis of size-resolved, laser-induced pa

6 In this study, we couple iron isotope analysis to microscopic and mineralogical i

7 The excretory pattern of the iron isotopes and the rare earth elements was very simil

8 ersuartuut, Greenland, are enriched in heavy iron isotopes by 0.1 to 0.5 per mil per atomic mass unit

9 ctively coupled plasma-mass spectrometry and iron isotopes by thermal ionization quadrupole mass spec

10 Laboratory experiments demonstrate that iron isotopes can be chemically fractionated in the abse

11 a ferromanganese crust demonstrates that the iron isotope composition in North Atlantic Deep Water ha

12 The iron isotope composition of sedimentary pyrite has been

13 Here we present the first pore water iron isotope data from a passive-tectonic and semi-arid

14 Here we provide iron isotope evidence that the change in the ocean iron

15 We show that significant variations of iron isotopes exist in both terrestrial and extraterrest

16 These results demonstrate that iron isotopes fractionate during magmatic differentiatio

17 dings provide insight into the mechanisms of iron isotope fractionation and suggest that nonbiologica

18 s of iron bonds, we calculate an equilibrium iron isotope fractionation between silicate and iron und

19 es was carried out to investigate oxygen and iron isotope fractionation during the intracellular prod

20 We report analyses of iron isotopes in basalts from Kilauea Iki lava lake, Haw

21 urements of the relative abundances of three iron isotopes in meteoritic and terrestrial samples.

22 No detectable fractionation of iron isotopes in the bacterial magnetites was observed.

23 However, heavy iron isotopes measured in seawater have recently led to

24 onation line, showing that homogenization of iron isotopes occurred in the solar nebula before both p

25 have shown for major elements like nitrogen, iron isotopes offer a new window into our understanding

26 high-resolution transect of dissolved stable iron isotope ratios (delta(56)Fe) and iron concentration

27 on from a standard test meal by using stable-iron-isotope techniques.

28 absence of food with the use of dual stable-iron-isotope techniques.

29 In a separate study utilizing stable iron isotopes, the 40% group absorbed 30% of ingested Fe

30 A high-precision iron isotope time series for a ferromanganese crust demo

31 Variable and negative iron isotope values in pyrites older than about 2.3 Ga s

32 Between 2.3 and 1.8 Ga, positive iron isotope values of pyrite likely reflect an increase

33 ially over the past 6 million years and that iron isotope variations in the crust are closely correla

34 at nonbiological processes may contribute to iron isotope variations observed in sediments.

35 o isotope series indicates that the observed iron isotope variations predominantly reflect those of i

WebLSDに未収録の専門用語（用法）は "新規対訳" から投稿できます。