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利用取自树桩的日本雪松年轮中的硫同位素比率对日本工业化时期的硫沉积特征进行表征。

Characterization of sulfur deposition over the period of industrialization in Japan using sulfur isotope ratio in Japanese cedar tree rings taken from stumps.

作者信息

Ishida Takuya, Tayasu Ichiro, Takenaka Chisato

机构信息

Laboratory of Forest Environment and Resources, Graduate School of Bioagricultural Sciences, Nagoya University, Furo-cho, Chikusa-ku, Nagoya, Aichi, 464-8601, Japan,

出版信息

Environ Monit Assess. 2015 Jul;187(7):459. doi: 10.1007/s10661-015-4678-0. Epub 2015 Jun 25.

Abstract

We characterized the sulfur deposition history over the period of industrialization in Japan based on the sulfur isotope ratio (δ(34)S) in tree rings of Japanese cedar (Cryptomeria japonica D. Don) stumps. We analyzed and compared δ(34)S values in the rings from two types of disk samples from 170-year-old stumps that had been cut 5 years earlier (older forest stand) and from 40-year-old living trees (younger forest stand) in order to confirm the validity of using stump disks for δ(34)S analysis. No differences in δ(34)S values by age were found between the sample types, indicating that stump disks can be used for δ(34)S analysis. The δ(34)S profile in tree rings was significantly correlated with anthropogenic SO2 emissions in Japan (r = -0.76, p < 0.05) and, thus, tree rings serve as a record of anthropogenic sulfur emissions. In addition, the values did not change largely from pre-industrialization to the 1940s (+4.2 to +6.1‰). The values before the 1940s are expected to reflect the background sulfur conditions in Japan and, thus, disks containing rings formed before the 1940s contain information about the natural environmental sulfur, which is useful for biogeochemical studies.

摘要

我们基于日本柳杉(Cryptomeria japonica D. Don)树桩年轮中的硫同位素比率(δ(34)S),描绘了日本工业化时期的硫沉积历史。我们分析并比较了来自两类圆盘样本年轮中的δ(34)S值,一类样本取自5年前砍伐的170年树龄的树桩(老龄林分),另一类取自40年树龄的活树(幼龄林分),以确认使用树桩圆盘进行δ(34)S分析的有效性。样本类型之间未发现δ(34)S值随树龄的差异,这表明树桩圆盘可用于δ(34)S分析。年轮中的δ(34)S剖面与日本人为SO2排放显著相关(r = -0.76,p < 0.05),因此,年轮可作为人为硫排放的记录。此外,从工业化前到20世纪40年代,这些值变化不大(从+4.2‰到+6.1‰)。预计20世纪40年代之前的值反映了日本的背景硫状况,因此,包含20世纪40年代之前形成年轮的圆盘含有有关自然环境硫的信息,这对生物地球化学研究很有用。

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