English (United Kingdom)

https://curated-unify.zendy.io/wp-json/zendy-region/v1/featured_content/oa?rat=en

https://curated-unify.zendy.io/wp-json/zendy-region/v1/highlighted_journal/

Global: Zendy Plus annual

Presents the access of premium content as premium feature

Premium Content

Presents the keyphrase highlighting as premium feature

Keyphrase Highlighting

Presents the summarisation as premium feature

Summarisation

Insights

Presents the pdf analysis as premium feature

PDF Analysis

Presents the zaia usage as premium feature

ZAIA

Global: Zendy Tools annual

Global: Zendy Free Plan

Global: Zendy Tools monthly

Global: Zendy Plus monthly

Mass-specific optical absorption coefficients (MACs) and the imaginary part(κ) of the refractive indices of various mineral dust componentsincluding silicate clays (illite, kaolin and bentonite), oxides (quartz,hematite and rutile), and carbonate (limestone) were determined at thewavelengths of 1064, 532, 355 and 266 nm. The MAC values were calculatedfrom aerosol optical absorption coefficients measured by a multi-wavelengthphotoacoustic (PA) instrument, the mass concentration and the number sizedistribution of the generated aerosol samples as well as the size transferfunctions of the measuring instruments. Values of  κ were calculatedfrom the measured and particle-loss-corrected data by using a Mie-theory-based retrieval algorithm. The determined values could be used forcomparisons with calculated wavelength-dependent κ values typicallydeduced from bulk-phase measurements by using indirect measurement methods.Accordingly, the presented comparison of the measured and calculated aerosoloptical absorption spectra revealed the strong need for standardized samplepreparation and measurement methodology in case of bulk-phase measurements

atmospheric measurement techniques

Mass-specific optical absorption coefficients and imaginary part of the complex refractive indices of mineral dust components measured by a multi-wavelength photoacoustic spectrometer