Analysis of double-emulsion droplets with ESI mass spectrometry for monitoring lipase-catalyzed ester hydrolysis at nanoliter scale.

Microfluidic double-emulsion droplets allow the realization and study of biphasic chemical processes such as chemical reactions or extractions on the nanoliter scale. Double emulsions of the rare type (o1/w/o2) are used here to realize a lipase-catalyzed reaction in the non-polar phase. The surrounding aqueous phase induces the transfer of the hydrophilic product from the core oil phase, allowing on-the-fly MS analysis in single double droplets. A microfluidic two-step emulsification process is developed to generate the (o1/w/o2) double-emulsion droplets. In this first example of microfluidic double-emulsion MS coupling, we show in proof-of-concept experiments that the chemical composition of the water layer can be read online using ESI-MS. Double-emulsion droplets were further employed as two-phase micro-reactors for the hydrolysis of the lipophilic ester p-nitrophenyl palmitate catalyzed by the Candida antarctica lipase B (CalB). Finally, the formation of the hydrophilic reaction product p-nitrophenol within the double-emulsion droplet micro-reactors is verified by subjecting the double-emulsion droplets to online ESI-MS analysis.

Degradation and adsorption of synthetic DNA water tracers in environmental matrices.

Synthetic DNA tracers are gaining interest as tools for tracking contamination pathways and hydraulic connections in surface water and groundwater systems. However, few quantitative data exist that describe DNA tracer degradation and adsorption in environmental matrices. We undertook laboratory experiments to quantify the degradation of multiple double-stranded DNA tracers in stream water, groundwater, and domestic and dairy-shed effluent, and adsorption to stream sediments, soils, coastal sand aquifer media and alluvial sandy gravel aquifer media. Faster DNA tracer degradation seemed to be associated with high bacterial concentrations in the liquid phase. Overall, the degradation of the 352 base pair (bp) DNA tracers in the aqueous phase was significantly (P = 0.018) slower than that of the 302 bp DNA tracers. Although the tracers' internal amplicon lengths were similar, the longer non-amplified flanking regions of the 352 bp tracers may better protect them from environmental degradation. Thermodynamic analysis suggests that longer flanking regions contribute to greater tracer stability. This finding may explain our previous field observations that 352 bp tracer mass reductions were often lower than 302 bp tracer mass reductions. The 2 sets of DNA tracers did not differ significantly regarding their adsorption to stream sediment-stream water or aquifer media-groundwater mixtures (P > 0.067), but the 352 bp tracers showed significantly less adsorption to soil-effluent mixtures than the 302 bp tracers (P = 0.005). The DNA tracers' adsorption to soil-effluent mixtures was comparatively less than their adsorption to the aquifer media-groundwater and stream sediment-stream water mixtures, suggesting that DNA tracers may compete with like-charged organic matter for adsorption sites. These findings provide insights into the fate of DNA tracers in the environment. The DNA tracers' degradation rate constants determined in this study for a range of environmental conditions could assist the design of future field investigations.

Water tracking in surface water, groundwater and soils using free and alginate-chitosan encapsulated synthetic DNA tracers.

Investigating contamination pathways and hydraulic connections in complex hydrological systems will benefit greatly from multi-tracer approaches. The use of non-toxic synthetic DNA tracers is promising, because unlimited numbers of tracers, each with a unique DNA identifier, could be used concurrently and detected at extremely low concentrations. This study aimed to develop multiple synthetic DNA tracers as free molecules and encapsulated within microparticles of biocompatible and biodegradable alginate and chitosan, and to validate their field utility in different systems. Experiments encompassing a wide range of conditions and flow rates (19 cm/day-39 km/day) were conducted in a stream, an alluvial gravel aquifer, a fine coastal sand aquifer, and in lysimeters containing undisturbed silt loam over gravels. The DNA tracers were identifiable in all field conditions investigated, and they were directly detectable in the stream at a distance of at least 1 km. The DNA tracers showed promise at tracking fast-flowing water in the stream, gravel aquifer and permeable soils, but were unsatisfactory at tracking slow-moving groundwater in the fine sand aquifer. In the surface water experiments, the microencapsulated DNA tracers' concentrations and mass recoveries were 1-3 orders of magnitude greater than those of the free DNA tracers, because encapsulation protected them from environmental stressors and they were more negatively charged. The opposite was observed in the gravel aquifer, probably due to microparticle filtration by the aquifer media. Although these new DNA tracers showed promise in proof-of-concept field validations, further work is needed before they can be used for large-scale investigations.