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Wavelet analysis of wintertime and spring thaw COd2 and Nd2O fluxes from agricultural fields

机译:农用地冬季和春季融化COd2和Nd2O通量的小波分析

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Fluxes of Nd2O and COd2 are not limited to the growing season; winter and spring thaw can represent a significant emission period. The objective of this study was to apply wavelet analysis to winter and spring thaw COd2 and Nd2O fluxes and soil temperatures, to yield additional information about underlying processes, examining temporal patterns and relationships among them. Fluxes used in this analysis were measured over 4 years using micrometeorological methods, in a study comparing two agricultural management practices, best management (BM) and conventional (CONV) practices. Cross-wavelet transform (XWT) and wavelet coherence (WCO) were applied to daily mean time series of Nd2O fluxes for BM and CONV replicates and treatments, COd2 vs. Nd2O fluxes, COd2 flux vs. air and soil temperatures, and Nd2O flux vs. air and soil temperatures. Nd2O fluxes for replicate plots had small differences in temporal variation while Nd2O fluxes from BM and CONV treatments showed a large difference in their time series. XWT and WCO analysis confirmed differences in Nd2O fluxes between management practices due to differences in temporal trends in the time series. Field emissions of Nd2O and COd2 fluxes showed times of common high fluxes, such as thaw events. Nitrous oxide and COd2 flux time series showed a strong coherence with surface (air) temperatures. The relationship between Nd2O fluxes and temperature decreased with depth but the relationship between COd2 flux and temperature was similar for surface and at depth. The strong coherence between emissions and surface conditions does not support the suggested mechanism of trapped gas release. A release of trapped gases from below the ice formation would have been indicated by a strong coherence from COd2 and Nd2O with temperatures at depth as the trapping ice barrier melted. This study demonstrates the effectiveness of wavelets as a tool to investigate temporal relationships in GHG emissions, which is a relatively new application for this type of analysis.
机译:Nd2O和COd2的流量不限于生长季节;冬季和春季解冻可代表一个重要的排放期。这项研究的目的是将小波分析应用于冬季和春季融化的COd2和Nd2O通量以及土壤温度,以产生有关基础过程的更多信息,检查时间模式及其之间的关系。在这项研究中,使用微气象学方法对通量进行了4年的测量,在一项研究中比较了两种农业管理实践,即最佳管理(BM)和常规(CONV)实践。将交叉小波变换(XWT)和小波相干性(WCO)应用于BM和CONV复制和处理的Nd2O通量的每日平均时间序列,COd2与Nd2O通量,COd2通量与空气和土壤温度以及Nd2O通量与空气和土壤温度。复制样区的Nd2O通量在时间变化上差异很小,而BM和CONV处理的Nd2O通量在时间序列上差异很大。 XWT和WCO分析证实,由于时间序列时间趋势的差异,管理实践之间Nd2O通量的差异。 Nd2O和COd2通量的场发射显示出常见的高通量的时间,例如解冻事件。一氧化二氮和COd2通量时间序列与表面(空气)温度具有很强的一致性。 Nd2O通量与温度之间的关系随深度而减小,而COd2通量与温度之间的关系在表面和深度上相似。排放物与表面条件之间的强一致性不支持所建议的捕获气体释放的机制。在结冰屏障融化时,COd2和Nd2O在深处的温度具有很强的连贯性,这表明结冰气体从冰层下方释放出来。这项研究证明了小波作为研究温室气体排放中时间关系的工具的有效性,这是此类分析的一个相对较新的应用。

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