森林土壤中素甲氧基组的同位素分析 (δ13C和 δ2H),以确定和量化素来源
Terry Cox1, Anna Wieland2, Markus Greule2
1Department of Environmental Sciences, University of Basel, Bernoullistrasse 30, 4056 Basel, Switzerland.
The Science of the total environment
|July 26, 2024
概括
在Lignin的基础上.
科学领域:
- 土壤科学 土壤科学
- 生物地质化学生物地质化学
- 有机化学 有机化学
背景情况:
- 土壤有机物 (SOM) 的形成受碳源分配的影响.
- 植物中丰富的红素对SOM至关重要,但其来源尚不清楚.
- 复杂的红素结构阻碍了对其对SOM的贡献的分析.
研究的目的:
- 在对比的土壤类型中调查红素源对SOM的贡献.
- 应用双同位素分析的素甲氧基 (LMeO) 的来源分配.
- 评估红素来源转移对碳循环模型的影响.
主要方法:
- 对LMeO的双同位素分析 (δ13C和δ2H) 的新应用.
- 使用贝叶斯混合模型 (MixSIAR) 来进行源分配.
- 在podzol和stagnosol土壤类型中分析了素来源.
主要成果:
- δ2H LMeO值区分在地面上方/下方的地面红素来源.
- δ13C LMeO 值区分了光合作用和非光合作用组织.
- 叶子垃圾的红素随着降解而减少;根红素占主导地位.
- 波兹罗尔阿赫的地平线积累了地面上方的木质红素.
- 14% (stagnosol) 和11% (podzol) 的散装13C缩归因于LMeO来源的转移.
结论:
- 对LMeO的双同位素分析有效地分配了红素来源.
- 素来源的贡献因土壤类型,降解和深度而异.
- 使用13C丰富的模型可能会高估碳循环,因为素来源的转移.
相关概念视频
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