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Fine-mode dust and fine sea salt emissions are weak contributors to PM2.5 mass throughout the continent with typical mass concentrations below 1 μg/m.
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It's already everywhere, like salt or CO2 emissions, so there's no need to overdo it.
When a 2-fold decline in ABA corolla levels of these plants was induced by salt stress, BA emissions recovered to WT levels.
Neither model includes salt or dust emissions, though dust and sea salt were estimated by comparing combustion-derived PM2.5 from TM5-FASST with APM2.5 estimates developed for GBD 2010 (Brauer et al. 2012) and used in the burden estimates (Lim et al. 2012).
Sulfate in snow and corresponding glacier ice can be derived from a variety of natural and anthropogenic sources such as sea-salt aerosols, biogenic emissions, entrained dust particles, fossil fuel combustion, and metal smelting.
The primary background PM10 included Sahara desert sand events, biogenic materials, mineral dust and sea salt aerosols, noninventoried Swiss emissions, and other anthropogenic particles from abroad.
The temporal variation of precipitation and relevant salinity fluctuation can significantly affect greenhouse gas (GHG) emissions of salt-affected soils in the Yellow River Delta (YRD) of China.
These luminescent pyridinium salts show weak emission in dichloromethane solutions at room temperature and a pronounced red-shifted emission in solid state.
In corollas of ir- hd20 plants, this fluctuation in ABA levels was not observed however when ABA levels in corollas were reduced by salt stress treatment, the emission of BA was recovered to WT levels.
Despite the common PET scaffold these benzimidazolium salts displayed diverse emission intensities in pure aqueous solutions.
However, salt stress conditions recovered BA emission in ir- hd20 plants and the levels of emitted BA were similar to those in WT plants.
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