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Tian, Q. et al. Microbial community mediated response of organic carbon mineralization to labile carbon and nitrogen addition in topsoil and subsoil.
Wang, Q. K., Wang, S. L., He, T. X., Liu, L. & Wu, J. B. Response of organic carbon mineralization and microbial community to leaf litter and nutrient additions in subtropical forest soils.
This provides a general method to improve sensor response of organic heterojunctions by controlling and tuning the film structure of sub-layer with appropriate fabrication techniques.
In this work, three dimensional finite element models of nacre (constructed in our previous work to design 'brick and mortar' micro-architecture of nacre) were used to study influence of nonlinear response of organic component.
The effective fluorescence response of organic dye to H2S and constant fluorescence of AuNCs enabled the proposed HSip-1@AuNC to achieve the ratiometric measurement with a dynamic linear range of 7 100 μM and a detection limit of 0.73 μM.
Efforts were targeted at elucidating organic-N structural criteria influencing the response of organic amines to known colorimetric and fluorescent reagents and exploring the use of divalent metal-assisted amide hydrolysis in combination with fluorescence analyses.
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Our study provides insights into the optical and structural response of organic-inorganic perovskite materials upon humidity exposure.
Short-lived metamorphism is further supported by the response of organics in naturally heated carbonaceous chondrites (Yabuta et al. 2010; Orthous-Daunay et al. 2013).
This study establishes predictable organic chemical responses of organic matter, upon exposure to ionising radiation.
In fact, the intrinsic response time of organic molecules is between 10 and 100 terahertz, meaning that if the right material is found, data might be processed at those astonishing speed.
Hu, L. N. et al. Response of soil organic carbon mineralization in typical Karst soils following the addition of 14C-labeled rice straw and CaCO3.
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