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沉积和土壤有机碳的升温热解放射性碳测年的空白校正

Blank corrections for ramped pyrolysis radiocarbon dating of sedimentary and soil organic carbon.

作者信息

Fernandez Alvaro, Santos Guaciara M, Williams Elizabeth K, Pendergraft Matthew A, Vetter Lael, Rosenheim Brad E

机构信息

Department of Earth and Environmental Science, Tulane University , New Orleans, Louisiana 70118, United States.

出版信息

Anal Chem. 2014 Dec 16;86(24):12085-92. doi: 10.1021/ac502874j. Epub 2014 Dec 4.

Abstract

Ramped pyrolysis (RP) targets distinct components of soil and sedimentary organic carbon based on their thermochemical stabilities and allows the determination of the full spectrum of radiocarbon ((14)C) ages present in a soil or sediment sample. Extending the method into realms where more precise ages are needed or where smaller samples need to be measured involves better understanding of the blank contamination associated with the method. Here, we use a compiled data set of RP measurements of samples of known age to evaluate the mass of the carbon blank and its associated (14)C signature, and to assess the performance of the RP system. We estimate blank contamination during RP using two methods, the modern-dead and the isotope dilution method. Our results indicate that during one complete RP run samples are contaminated by 8.8 ± 4.4 μg (time-dependent) of modern carbon (MC, fM ∼ 1) and 4.1 ± 5.5 μg (time-independent) of dead carbon (DC, fM ∼ 0). We find that the modern-dead method provides more accurate estimates of uncertainties in blank contamination; therefore, the isotope dilution method should be used with caution when the variability of the blank is high. Additionally, we show that RP can routinely produce accurate (14)C dates with precisions ∼100 (14)C years for materials deposited in the last 10,000 years and ∼300 (14)C years for carbon with (14)C ages of up to 20,000 years.

摘要

阶梯升温热解(RP)基于土壤和沉积有机碳的热化学稳定性,针对其不同组分进行分析,并能够测定土壤或沉积物样品中存在的全谱放射性碳(¹⁴C)年龄。将该方法扩展到需要更精确年龄或需要测量更小样品的领域,需要更好地了解与该方法相关的空白污染情况。在此,我们使用一组已知年龄样品的RP测量汇编数据集,来评估碳空白的质量及其相关的¹⁴C特征,并评估RP系统的性能。我们使用现代-死碳法和同位素稀释法两种方法来估算RP过程中的空白污染。我们的结果表明,在一次完整的RP运行过程中,样品受到8.8±4.4μg(随时间变化)的现代碳(MC,fM1)和4.1±5.5μg(与时间无关)的死碳(DC,fM0)的污染。我们发现,现代-死碳法能更准确地估计空白污染的不确定性;因此,当空白的变异性较高时,应谨慎使用同位素稀释法。此外,我们表明,对于过去10000年沉积的材料,RP通常可以常规地产生精度约为100¹⁴C年的准确¹⁴C年代,对于¹⁴C年龄高达20000年的碳,精度约为300¹⁴C年。

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