11 research outputs found

    Vertical Distributions of Radionuclides (<sup>239+240</sup>Pu, <sup>240</sup>Pu/<sup>239</sup>Pu, and <sup>137</sup>Cs) in Sediment Cores of Lake Bosten in Northwestern China

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    Artificial radionuclides (<sup>137</sup>Cs, <sup>239+240</sup>Pu, <sup>241</sup>Pu, <sup>241</sup>Am) deposited in lacustrine sediments have been used for dating as well as radionuclide source identification. In the present work, we investigated the vertical distributions of <sup>239+240</sup>Pu and <sup>137</sup>Cs activities, <sup>240</sup>Pu/<sup>239</sup>Pu atom ratios, and <sup>239+240</sup>Pu/<sup>137</sup>Cs activity ratios in sediment cores collected from Lake Bosten, which is the lake closest to the Lop Nor Chinese Nuclear Weapon Test site in northwestern China. Uniformly high concentrations of <sup>239+240</sup>Pu and <sup>137</sup>Cs were found in the upper layers deposited since 1964 in the sediment cores, and these were controlled by the resuspension of soil containing radionuclides from the nearby land surface. As the Chinese nuclear tests varied remarkably in yield, the mixing of the tropospheric deposition from these tests and the stratospheric deposition of global fallout has led to a <sup>240</sup>Pu/<sup>239</sup>Pu atom ratio that is similar to that of global fallout and to a <sup>239+240</sup>Pu/<sup>137</sup>Cs activity ratio that is slightly higher than that of global fallout. However, a low <sup>240</sup>Pu/<sup>239</sup>Pu atom ratio of 0.080 and high <sup>239+240</sup>Pu/<sup>137</sup>Cs activity ratio of 0.087, significantly different from the global fallout values, were observed in one sediment core (07BS10-2), indicating the inhomogenous tropospheric deposition from the Chinese nuclear tests in Lake Bosten during 1967–1973. These results are important to understand the influence of the CNTs on the radionuclide contamination in Lake Bosten

    Analyses of peroxidase activities of OxdAs in the presence of ABTS.

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    <p>(A) The peroxidase activities of OxdAs depending on the H<sub>2</sub>O<sub>2</sub> concentration. OxdA(WT) [(a) black circles], OxdA(H320D) [(a) black triangles], and OxdA(H320A) [(b) black square]. (B) Michaelis—Menten kinetics of the peroxidase activity of OxdAs. OxdA(WT) (a), OxdA(H320D) (b) and OxdA(H320A) (c). The reactions with ABTS as a substrate were carried out under the “standard assay C” conditions as described under “Materials and Methods.” For all data points, values are means ± mean error.</p

    Analyses of peroxidase activities of OxdAs in the presence of guaiacol.

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    <p>(A) The peroxidase activities of OxdAs depending on the H<sub>2</sub>O<sub>2</sub> concentration. OxdA(WT) [(a) black circles], OxdA(H320D) [(a) black triangles], and OxdA(H320A) [(b) black square]. (B) Michaelis—Menten kinetics of the peroxidase activity of OxdAs. OxdA(WT) (a), OxdA(H320D) (b) and OxdA(H320A) (c). The reactions with guaiacol as a substrate were carried out under the “standard assay B” conditions as described under “Materials and Methods.” For all data points, values are means ± mean error.</p

    Michaelis—Menten kinetics of the catalase activity of OxdAs.

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    <p>The reactions were carried out under the “standard assay A” conditions as described under “Materials and Methods.” For all data points, values are means ± mean error. OxdA(WT) (A), OxdA(H320D) (B) and OxdA(H320A) (C).</p
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