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T Sotobayashi

Publications and source records attributed to T Sotobayashi.

14 recordsLinked to original sources

Purification and properties of an auxin-binding protein from maize shoot membranes.

An auxin-binding protein was purified from membranes of maize shoots including the coleoptiles, leaf rolls and mesocotyls. The method of Ca2+-promoted sedimentation of membrane particles was adopted for large-scale preparation. The auxin-binding protein was solubilized from the acetone-washed membranes, and purified by successive chromatographies on DEAE-Sephacel, 1-naphthylacetic acid-linked AH-Sepharose 4B, and Sephadex G-100 columns. The yield of the purified protein was about 0.2 mg from 1 kg of shoots. The binding protein exists as a dimer with a subunit molecular weight of 21,000, and possesses one auxin-binding site per dimer. The preparation also contains a minor molecular form with a subunit molecular weight of 20,000. The auxin-binding protein is not a hydrophobic protein, as judged from its amino acid composition and solubility. The circular dichroic (CD) spectrum of the binding protein resembles the spectrum anticipated from the beta-structures, and shows no alpha-helix characteristic in the secondary structure. The CD spectral changes induced on the binding of auxin and its antagonist seem to be related to the receptor function. The affinity of the binding protein for auxin is dependent on pH, with an optimum at pH 5.0, while the binding protein is unstable below pH 6. We discuss here the intracellular localization of the auxin-binding protein from the view point of the controversial pH-dependence of the binding affinity and stability.

Amino Acids↗

[Dosimetric application of lyoluminescence using some saccharides].

A measurement system for lyoluminescence has been constructed using a photon-counting apparatus equipped with a highly sensitive photomultiplier and a microcomputer for a data acquisition and processing. For the lyoluminescent dosimetry, seven saccharide samples, including five monosaccharides (glucose, mannose, galactose, levulose and ribose) and two disaccharides (sucrose and trehalose), were irradiated with 60Co gamma rays. Effects on lyoluminescence were examined of the amounts of the sample, concentration of luminol phosphor in an aqueous solution, elapsed time after mixing the samples in the solution, variations of absorbed doses, annealing treatments and different radiation fields. The results revealed that relatively small amounts of sample, say 3 mg, is sufficient for reproducible routine analyses by using 125 mg luminol/l for 10 s data accumulation, and that the lyoluminescent dosimetry is useful for the significantly high dose regions of 1Gy-10kGy (the use of galactose and trehalose can extend the dose-region to higher levels). The comparison of sensitivity for samples with the same dose (215 Gy) showed the great luminescent changes over one order of magnitude between the highest value for galactose and lowest one for ribose, although there is no substantial difference in the structure. No meaningful radiation-quality effect was observed for monosaccharides irradiated with gamma-rays, X-rays, and neutrons.

Carbohydrates↗

[Alpha-recoiling behaviour of 222Rn on 226Ra-sources].

By using electroplated 226Ra-sources, the ejection and injection behaviour of alpha-recoil atoms, 222Rn, which generates on the source surface during alpha-decay process of its parent 226Ra, has been basically investigated. The thinly and uniformly distributed 226Ra-sources were prepared with high deposition yield by the molecular plating technique, in which radium was deposited on a stainless-steel cathode from an isopropanol media by adopting a rotating platinum anode, applied potential of 900 V, and deposition time of 40 min. The ejection efficiency of 222Rn was determined by using the relationship between the 226Ra strength on source and the 222Rn-one transferred on a stainless steel collector in vacuum. It was found that the ejection (or injection) efficiency was greatly influenced on the source preparation methods. The highest ejection efficiency (up to 30%) could be obtained from the electroplated source, whereas the same source could be resulted in the significant decrease of this value (till 2%) after simple ignition treatment. The retention efficiency of 222Rn injected on some collector materials was evaluated to be more than 70% over the tested collectors. From these results, it was concluded that the recoil effects should be most important to interpret the emanation phenomena even in nature.

Alpha Particles↗

[New color-photographic observation of thermoluminescence of sliced rock samples].

New observation technique has been established for the thermoluminescence photography using extremely high-sensitive color films. Considering future application to the geological fields, a granite was selected as a testing material. The sliced specimens (0.5- 0.7 mm in thickness), which were irradiated with a 60Co source, were mounted on the heater attached with a thermocouple, which was connected to a microcomputer for measuring the temperature. The samples were heated in the temperature range of 80-400 degrees C by operating the camera-shutter controlled with the microcomputer. Four commercially available films (Kodak-1000(ASA), -400, Sakura-400, Fuji-400) could give apparently detectable color-images of artificial thermoluminescence above a total absorbed dose of 880 Gy(88 krad). The specimens, irradiated upto 8.4 kGy(840 krad), allowed easily to distinguish the distinct appearance of the thermoluminescence images depending on kinds of white mineral constituents. Moreover, such color images were changeable with the heating temperature. Sakura-400 film has proved the most colorful images from aspects of color tone although Kodak-1000 film showed the highest sensitivity. By applying this Kodak-1000, it was found that the characteristic color image due to natural thermoluminescence was significantly observed on the Precambrian granite which was exposed with natural radiation alone since its formation. This simple and interesting technique, obtainable surface information reflecting impurities and local crystal defects in addition to small mineral constituents, was named as the thermoluminescence color imaging (abbreviated to TLCI) technique by the authors and its versatile applications were discussed.

Color↗

[Alpha-spectroscopic determination of 210Pb and 210PO in snow samples].

The concentrations of 210Pb and 210PO in several snow samples were determined using alpha-spectrometry. After 5 l of snow-melt water was subjected to coprecipitation of both nuclides with AlPO4, the solvent extraction procedure with TBP (tri-butyl phosphate)-isopropyl ether was applied to purify the polonium fraction, followed by the spontaneous electro-deposition on a Ni-sheet. The alpha-spectrum was measured with a Si(Au)-semiconductor detector coupled with a multichannel pulse-height analyzer. After the first determination of 210PO, the concentration of 210Pb was estimated from second measurement of 210PO grown newly from the remaining Pb-fraction during the storage period of more than 3 months. In these analytical procedures, 212Pb and 208PO tracers were conveniently utilized for the determination of collection yield for 210Pb and of the final chemical yield of 210PO, respectively. The contents of 210PO and 210Pb in the fresh snow were 3--30 mBq/l(81--810 fCi/l) and 250--720 mBq/l (6.8--19.5 pCi/l), respectively, and the residence time of 210Pb was given to be 6--12 days from the decay-growth relationships of both nuclides.

Alpha Particles↗

[Determination of uranium contents in fossil bones using fission track method--new counting method of fission tracks with high density].

Determination of the average uranium contents in several fossil bones was carried out using an improved fission track method. Four standard samples were prepared from silica-gel powder containing known amounts of natural uranium. The powdered fossil bones was fixed on a muscovite detector as well as the standard samples and followed by the neutron irradiation. After cooling, the muscovites were chemically etched with HF-solution to develop the fission tracks. By using standard samples, it was found that a reliable track counting is impossible through the transmission optical microscope in the region over track density of 5 X 10(5) cm-2 because of overlap of fission tracks in each other. In order to improve this situation bearing most of the present muscovites, the observation using the reflection microscope was applied after coating the muscovite surface with the vacuum-evaporated gold film and verified to be extremely efficient to the counting of high track density up to 5 X 10(7) cm-2, which could be no longer to distinguish intrinsic tracks through ordinary microscope. All of the fossil samples were subjected to the track counting through the reflection microscope and after correcting the estimated difference of track ranges between the standard and fossil bone samples the experimental uranium contents were evaluated. The uranium contents in the fossil bones were in the range of 30-460 ppm.

Animals↗

[Determination of natural radioactive nuclides in the travertine samples from Tamagawa hot spring].

The determination of natural radioactive nuclides was carried out for 7 travertine samples collected from Tamagawa hot spring by means of the non-distructive gamma-ray spectrometry and of the alpha-ray spectrometry. From the former measurements, the relative activity strength, due to 223Ra, 226Ra, and 228Th, and their ratios was obtained in comparison with the photopeak strength due to respective daughters, 228Ac, 214Bi, and 212Pb, and with the results from a monazite sand standard. One travertine sample was engaged to the alpha-ray spectrometric determination of Th isotopes after the chemical purification using a 234Th-yield tracer. On the basis of the resultant absolute content of 228Th, the 228Ra and 228Th contents in the remainder samples were evaluated to be the range of 3 approximately 80 Bq (81 approximately 2160 pCi)/g and 2 approximately 20 Bq (54 approximately pCi)/g respectively. These radioactive nuclides were verified to exist almost within a Hokutolite small crystals up to 90% and there are apparently the radioactive disequilibrium relations between 228Ra and 228Th among freshly deposited travertines. The presence of 227Ac in Hokutolite was also suggested from the detection of 227Th owing to 215Po-alpha peak.

Japan↗

Stontium-90 fallout from surface and underground nuclear tests.

Deposition of strontium-90 per unit area per unit fission energy from surface blast of the first Chinese atomic bomb was several times heavier than that from an earlier atmospheric test series. The venting of a Russian large-scale underground test also significantly increased deposition of strontium-90 at Niigata, Japan.

China↗