Although most of researchers agree on the elementary reactions behind the sonolytic formation of molecular hydrogen (H) from water, namely the radical attack of HO and HO and the free radicals recombination, several recent papers ignore the intervention of the dissolved gas molecules in the kinetic pathways of free radicals, and hence may wrongly assess the effect of dissolved gases on the sonochemical production of hydrogen. One may fairly ask to which extent is it acceptable to ignore the role of the dissolved gas and its eventual decomposition inside the acoustic cavitation bubble? The present opinion paper discusses numerically the ways in which the nature of dissolved gas, i.e., N, O, Ar and air, may influence the kinetics of sonochemical hydrogen formation. The model evaluates the extent of direct physical effects, i.e., dynamics of bubble oscillation and collapse events if any, against indirect chemical effects, i.e., the chemical reactions of free radicals formation and consequently hydrogen emergence, it demonstrates the improvement in the sonochemical hydrogen production under argon and sheds light on several misinterpretations reported in earlier works, due to wrong assumptions mainly related to initial conditions. The paper also highlights the role of dissolved gases in the nature of created cavitation and hence the eventual bubble population phenomena that may prevent the achievement of the sonochemical activity. This is particularly demonstrated experimentally using a 20 kHz Sinaptec transducer and a Photron SA 5 high speed camera, in the case of CO-saturated water where degassing bubbles are formed instead of transient cavitation.
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http://dx.doi.org/10.1016/j.ultsonch.2020.105422 | DOI Listing |
PLoS One
December 2024
Department of Earth and Environmental Sciences, Vanderbilt University, Nashville, Tennessee, United States of America.
Monitoring the seasonal and diurnal variations in headwater stream metabolic regimes can provide critical information for understanding how ecosystems will respond to future environmental changes. In East Fork Creek, a headwater stream in middle Tennessee, week-long field campaigns were set up each month from May 2022 to May 2023 to collect stream metabolism estimators. In a more extensive field campaign from July 2-5 in 2022, diel signals were observed for temperature, pH, turbidity, and concentrations of Ca, Mg, K, Se, Fe, Ba, chloride, nitrate, DIC, DO, DOC, and total algae.
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December 2024
Department of Integrative Biology, Oregon State University, Corvallis, OR, 97331, USA.
The supply of nitrogen (N) and the efficiency with which it is used by phytoplankton serve as two fundamental controls on the productivity of many marine ecosystems. Shifts in nitrogen use efficiency (NUE) can decouple primary production from N-supply but how NUE varies across systems is poorly known. Through a global synthesis of how total N (TN) is apportioned among phytoplankton, particulate, dissolved inorganic, and dissolved organic pools, we demonstrate that NUE underlies broad variations in primary production.
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December 2024
Wushan County Productivity Promotion Center, Tianshui, 741300, China.
Soil nitrogen (N) transformation is an essential portion of the N cycle in wetland ecosystems, governing the retention status of soil N by controlling the effective soil N content. N deposition produced by human activities changes the physical characteristics of soil, affecting N fractions and enzyme activities. To characterize these influences, three different N addition levels (N5, 5 g/m; N10, 10 g/m; N15, 15 g/m) were established using a wet meadow on the Qinghai-Tibet Plateau (QTP) as a control treatment (0 g/m).
View Article and Find Full Text PDFLangmuir
December 2024
Institute of Physics, Academia Sinica, Nankang, Taipei 115, Taiwan.
In the present study, we deposited buffer solutions containing hydrophobic (GA) fibrils onto highly oriented pyrolytic graphite (HOPG) and imaged the surfaces through atomic force microscopy (AFM). Within 3 h of applying ambient (nondegassed) buffers, we observed the formation of two-dimensional stripe-like domains on the HOPG surfaces surrounding the (GA) fibrils. However, these stripe domains did not form under degassed buffers.
View Article and Find Full Text PDFHuan Jing Ke Xue
January 2025
State Key Laboratory of Soil and Sustainable Agriculture, Institute of Soil Science, Chinese Academy of Sciences, Nanjing 210008, China.
In this investigation, the influence of organic amendment on the structural and functional dynamics of soil microbial communities and its effect on rice productivity were examined. Five fertilization treatments from a 40-year field experiment were selected: no fertilizer (CK), inorganic NPK fertilizer (NPK), inorganic NPK combined with green manure (NG), inorganic NPK combined with green manure and pig manure (NGM), and inorganic NPK combined with green manure and rice straw (NGS). The findings revealed that the organic amendment enhanced the soil organic carbon (SOC), total nitrogen (TN), and total phosphorus (TP) levels, alongside an increase in rice yield; notably, the most significant improvements were observed with the NGM treatment.
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