Organic carbon preservation in wetlands: Iron oxide protection vs. thermodynamic limitation.

The sequestration of organic carbon (OC) in wetland sediments is influenced by the presence of oxygen or lack thereof. The mechanisms of OC sequestration under redox fluctuations, particularly by the co-mediation of reactive iron (Fe) protection and thermodynamic limitation by the energetics of the OC itself, remain unclear. Over the past 26 years, a combination of field surveys and remote sensing images had revealed a strong decline in both natural and constructed wetland areas in Tianjin.

Global airborne bacterial community-interactions with Earth's microbiomes and anthropogenic activities.

Airborne bacteria are an influential component of the Earth's microbiomes, but their community structure and biogeographic distribution patterns have yet to be understood. We analyzed the bacterial communities of 370 air particulate samples collected from 63 sites around the world and constructed an airborne bacterial reference catalog with more than 27 million nonredundant 16S ribosomal RNA (rRNA) gene sequences. We present their biogeographic pattern and decipher the interlacing of the microbiome co-occurrence network with surface environments of the Earth.

[Effects of freeze-thaw and soil moisture on content and spectral structure properties of dissolved organic matter in forest soil leachates.].

The contents and stability of soil dissolved organic matter (DOM) can affect key processes of soil carbon and nitrogen cycle. The responses of DOM content and its spectral structure pro-perties in forest soils to climate change remain unclear. We collected soil samples from two temperate forests, i.

[Profile characteristics and seasonal variation of dissolved organic matter in Hongfeng Lake, Guizhou].

Dissolved organic carbon (DOC) and dissolved organic nitrogen (DON) are rarely measured together when studying dissolved organic matter (DOM) in lake water. DOC and DON concentrations were measured for a Karst plateau lake--Hongfeng Lake water for nearly two years. Profile characteristics and seasonal variation of dissolved organic matter were studied, and influencing factors were discussed.

[Effect of sunlight irradiation on fluorescence properties of dissolved organic matter].

Three-dimensional excitation emission matrix fluorescence spectroscopy (3DEEM) was used to investigate the effect of sunlight irradiation on the fluorescence properties of dissolved organic matter (DOM) from Lake Hongfeng and Nanming River waters and a commercial fluka humic acid (FHA). The results show that the DOM samples and FHA fluorescence properties changed under sunlight irradiation. Interestingly, the photodegradation characteristics were different between aquatic DOM and FHA.

[Three-dimensional excitation emission matrix fluorescence spectroscopic characterization of dissolved organic matter].

Three-dimensional excitation emission matrix fluorescence spectroscopy (3DEEM) was applied to characterize the fluorescence properties of dissolved organic matter (DOM) in lakes, rivers, streams, and ground waters. The results showed that the 3DEEM of DOM in aquatic environments mainly have four fluorescence peaks: peak A and C was referred to as fulvic-like fluorescence, and peak B and D was referred to as protein-like fluorescence. Results of river water DOM typically showed strong fulvic-like fluorescence.

[Three-dimensional excitation emission matrix fluorescence spectroscopic characterization of the complexation between mercury (II) and dissolved organic matter].

With the development of fluorescence technique, three-dimensional excitation emission matrix fluorescence spectroscopy (3DEEM) was widely applied to characterize the nature of dissolved organic matter (DOM) in natural waters since the last decade. 3DEEM and fluorescence quenching titration were used to study the interaction between Hg(II) and DOM. The results show that a general decrease in intensity for individual peak A, B and C was found as concentrations of Hg(II) increased.