The stable oxygen isotope ratio of resin extractable phosphate derived from fresh cattle faeces.

从新鲜牛粪中提取的树脂可提取磷酸盐的稳定氧同位素比值

阅读:3
作者:Granger Steven J, Yang Yuguo, Pfahler Verena, Hodgson Chris, Smith Andrew C, Le Cocq Kate, Collins Adrian L, Blackwell Martin S A, Howden Nicholas J K
RATIONALE: Phosphorus losses from agriculture pose an environmental threat to watercourses. A new approach using the stable oxygen isotope ratio of oxygen in phosphate (δ(18) O(PO4) value) may help elucidate some phosphorus sources and cycling. Accurately determined and isotopically distinct source values are essential for this process. The δ(18) O(PO4) values of animal wastes have, up to now, received little attention. METHODS: Phosphate (PO(4) ) was extracted from cattle faeces using anion resins and the contribution of microbial PO(4) was assessed. The δ(18) O(PO4) value of the extracted PO(4) was measured by precipitating silver phosphate and subsequent analysis on a thermal conversion elemental analyser at 1400°C, with the resultant carbon monoxide being mixed with a helium carrier gas passed through a gas chromatography (GC) column into a mass spectrometer. Faecal water oxygen isotope ratios (δ(18) O(H2O) values) were determined on a dual-inlet mass spectrometer through a process of headspace carbon dioxide equilibration with water samples. RESULTS: Microbiological results indicated that much of the extracted PO(4) was not derived directly from the gut fauna lysed during the extraction of PO(4) from the faeces. Assuming that the faecal δ(18) O(H2O) values represented cattle body water, the predicted pyrophosphatase equilibrium δ(18) O(PO4) (Eδ(18) O(PO4) ) values ranged between +17.9 and +19.9‰, while using groundwater δ(18) O(H2O) values gave a range of +13.1 to +14.0‰. The faecal δ(18) O(PO4) values ranged between +13.2 and +15.3‰. CONCLUSIONS: The fresh faecal δ(18) O(PO4) values were equivalent to those reported elsewhere for agricultural animal slurry. However, they were different from the Eδ(18) O(PO4) value calculated from the faecal δ(18) O(H2O) value. Our results indicate that slurry PO(4) is, in the main, derived from animal faeces although an explanation for the observed value range could not be determined.

特别声明

1、本页面内容包含部分的内容是基于公开信息的合理引用;引用内容仅为补充信息,不代表本站立场。

2、若认为本页面引用内容涉及侵权,请及时与本站联系,我们将第一时间处理。

3、其他媒体/个人如需使用本页面原创内容,需注明“来源:[生知库]”并获得授权;使用引用内容的,需自行联系原作者获得许可。

4、投稿及合作请联系:info@biocloudy.com。