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Assessing soil constituents and labile soil organic carbon by mid-infrared photoacoustic spectroscopy

机译:通过中红外光声光谱法评估土壤成分和不稳定的土壤有机碳

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Recent progress in microphone sensitivity has dramatically increased the performance of Fourier transform mid-infrared photoacoustic spectroscopy (FTIR-PAS). This technique offers benefits over reflectance spectroscopy techniques because the level of sample reflectance has little effect on the PAS signal. This also means that it should be advantageous for soil analysis because of its highly opaque nature. However, only a limited number of studies have so far applied FTIR-PAS to soil characterization and investigation is still required into its potential to determine soil organic carbon (SOC) degradability. The objective of this study was to assess the potential of FTIR-PAS for the characterisation of the labile fraction of SOC and more classical soil parameters, such as carbon and clay content, for a range of 36 soils collected from various field experiments in Denmark. Partial least squares (PLS) regression was used to correlate the collected FTIR-PAS spectra with the proportion of soil organic carbon mineralised after 238 days of incubation at 15 degrees C and pF 2 (C-238d) taken as an indicator of the labile fraction of SOC. Results showed that it is possible to predict total organic carbon content, total nitrogen content and the labile fraction of SOC using FTIR-PAS with an accuracy similar to or better than near infrared (NIR) spectroscopy. FTIR-PAS offered the advantage over NIR of allowing identification of chemical compounds that correlated positively or negatively with the labile fraction of SOC. Spectral bands corresponding to aliphatic, methyl, amide III and polysaccharides compounds were positively correlated with C-238d, whereas bands corresponding to aromatics, amines, amides II and carboxylic acids were negatively correlated with C-238d. In conclusion, FTIR-PAS has proved to be a powerful tool for characterising soil composition and its labile SOC fraction, offering several benefits over reflectance spectroscopy techniques
机译:麦克风灵敏度的最新进展极大地提高了傅里叶变换中红外光声光谱技术(FTIR-PAS)的性能。由于样品反射率的水平对PAS信号影响很小,因此该技术比反射光谱技术具有更多优势。这也意味着由于其高度不透明的特性,因此对土壤分析应该是有利的。但是,到目前为止,只有有限的研究将FTIR-PAS应用于土壤表征,并且仍需要对其确定土壤有机碳(SOC)降解性的潜力进行调查。这项研究的目的是评估FTIR-PAS在表征SOC的不稳定成分和更经典的土壤参数(如碳和粘土含量)方面的潜力,该方法可用于从丹麦的各种田间试验中收集到的36种土壤。使用偏最小二乘(PLS)回归将收集的FTIR-PAS光谱与在15摄氏度下孵育238天后矿化的土壤有机碳的比例相关,并将pF 2(C-238d)用作不稳定部分的指标SOC。结果表明,使用FTIR-PAS可以预测总有机碳含量,总氮含量和SOC的不稳定部分,其准确度与近红外(NIR)光谱相似或更好。与NIR相比,FTIR-PAS的优势在于可以鉴定与SOC不稳定部分呈正相关或负相关的化合物。对应于脂族,甲基,酰胺III和多糖化合物的光谱带与C-238d正相关,而对应于芳族化合物,胺,酰胺II和羧酸的谱带与C-238d负相关。总之,事实证明,FTIR-PAS是表征土壤成分及其不稳定SOC含量的有力工具,与反射光谱技术相比,具有许多优势

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