Dungait Jennifer A J, Stear Natalie A, van Dongen Bart E, Bol Roland, Evershed Richard P
Organic Geochemistry Unit, Bristol Biogeochemistry Research Centre, School of Chemistry, Cantocks Close, Bristol BS8 1TS, UK.
Rapid Commun Mass Spectrom. 2008 Jun;22(11):1631-9. doi: 10.1002/rcm.3454.
Off-line pyrolysis was used to liberate lignin moieties from dung and soil and, after trimethylsilylation, the delta(13)C values of these derivatives were determined by gas chromatography-combustion-isotope ratio mass spectrometry. Initial delta(13)C values determined for 4-vinylphenol, syringol, 4-vinylguaiacol, 4-acetylsyringol, 4-vinylsyringol, 4-(2-Z-propenyl)syringol, 4-(2-E-propenyl)syringol and 4-(2-propenone)syringol pyrolysis products of the lignin polyphenol structure from C(4) (delta(13)C(bulk) = -12.6%) and C(3) (delta(13)C(bulk) = -30.1 per thousand) dung confirmed the robust and reproducible nature of the off-line preparation technique. C(4) dung was used as a treatment in a randomised field experiment to assess the short-term sequestration of dung carbon in managed grasslands. Since lignin was on average 3.5 per thousand depleted in (13)C compared with bulk dung delta(13)C values, this may have resulted in an under-estimation of dung C incorporation based on bulk delta(13)C values. Therefore, an investigation of the compound-specific delta(13)C values of dung-derived lignin moieties extracted from soils sampled up to 372 days was undertaken. Delta(13)C values between lignin moieties extracted from treated and untreated soils showed that dung-derived lignin was not especially resistant to degradation and suggested that individual moieties of the lignin macromolecule must: (i) move into soil, (ii) be degraded, or (iii) be transformed diagenetically at different rates. This adds to a gathering body of evidence that lignin is not particularly stable in soils, which has considerable significance for the perceived role of different biochemical components in the cycling of C in soils.
离线热解用于从粪便和土壤中释放木质素部分,在进行三甲基硅烷化后,通过气相色谱 - 燃烧 - 同位素比率质谱法测定这些衍生物的δ(13)C值。对来自C(4)(δ(13)C(总体) = -12.6%)和C(3)(δ(13)C(总体) = -30.1‰)粪便的木质素多酚结构的4 - 乙烯基苯酚、丁香酚、4 - 乙烯基愈创木酚、4 - 乙酰丁香酚、4 - 乙烯基丁香酚、4 - (2 - Z - 丙烯基)丁香酚、4 - (2 - E - 丙烯基)丁香酚和4 - (2 - 丙烯酮)丁香酚热解产物测定的初始δ(13)C值证实了离线制备技术的稳健性和可重复性。C(4)粪便被用作随机田间试验中的一种处理,以评估管理草地上粪便碳的短期固存情况。由于与粪便总体δ(13)C值相比,木质素的(13)C平均贫化3.5‰,这可能导致基于总体δ(13)C值对粪便碳掺入量的低估。因此,对从长达372天采样的土壤中提取的粪便衍生木质素部分的化合物特异性δ(13)C值进行了研究。从处理过和未处理过的土壤中提取的木质素部分之间的δ(13)C值表明,粪便衍生的木质素对降解并非特别有抗性,并表明木质素大分子的各个部分必须:(i) 进入土壤,(ii) 被降解,或(iii) 以不同速率进行成岩转化。这增加了越来越多的证据表明木质素在土壤中并非特别稳定,这对于不同生化成分在土壤碳循环中所起的作用具有重要意义。