Abstract

Abstract. As Na+, Mg2+, and Cl− are major ionic constituents of seawater, NaCl–MgCl2 mixture particles might represent sea-spray aerosols (SSAs) better than pure NaCl. However, there have been very few hygroscopic studies of pure MgCl2 and NaCl–MgCl2 mixture aerosol particles despite the MgCl2 moiety playing a major role in the hygroscopic behavior of nascent SSAs. Laboratory-generated pure MgCl2 and NaCl–MgCl2 mixture aerosol particles with 12 mixing ratios (0.01 ≤ mole fraction of NaCl (XNaCl) ≤ 0.9) were examined systematically by optical microscopy (OM), in situ Raman micro-spectrometry (RMS), and scanning electron microscopy/energy dispersive X-ray spectrometry (SEM/EDX) elemental X-ray mapping to observe their hygroscopic behavior, derive the experimental phase diagrams, and obtain the chemical micro-structures. Dry-deposited MgCl2 ⋅ 6H2O particles exhibited a deliquescence relative humidity (DRH) of ~ 33.0 % and an efflorescence RH (ERH) of 10.8–9.1 %, whereas the nebulized pure MgCl2 and MgCl2-dominant particles of XNaCl = 0.026 (eutonic) and 0.01 showed single-stage transitions at DRH of ~ 15.9 % and ERH of 10.1–3.2 %. The characteristic OH-stretching Raman signatures indicated the crystallization of MgCl2 ⋅ 4H2O at low relative humidities (RHs), suggesting that the kinetic barrier to MgCl2 ⋅ 6H2O crystallization is not overcome in the timescale of the dehydration measurements. The NaCl–MgCl2 mixture particles of 0.05 ≤ XNaCl ≤ 0.9 generally showed two-stage deliquescence: first at the mutual DRH (MDRH) of ~ 15.9 %; and second with the complete dissolution of NaCl at the second DRHs depending on the mixing ratios, resulting in a phase diagram composed of three distinct phases. During dehydration, most particles of 0.05 ≤ XNaCl ≤ 0.9 exhibited two-stage efflorescence: first, by the homogeneous nucleation of NaCl; and second, at mutual ERH (MERH) of ~ 10.4–2.9 %, by the crystallization of the MgCl2 ⋅ 4H2O moiety, also resulting in three distinct phases. Interestingly, particles of XNaCl = 0.1 and 0.2 frequently showed three different types of mutual deliquescence behaviors. The first type exhibited an MDRH at ~ 15.9 %. The second exhibited the first MDRH at ~ 15.9 %, efflorescence to MgCl2 ⋅ 6H2O (confirmed by in situ RMS) at RH of ~ 16.1–25.0 %, and a second MDRH at ~ 33.0 %. The third showed an MDRH at ~ 33.0 %. Some particles of XNaCl = 0.1 and 0.2 also exhibited higher MERHs = 15.2–11.9 % and 23.7–15.3 %, respectively, forming MgCl2 ⋅ 6H2O. These observations suggest that the presence of sufficient condensed water and optimally sized crystalline NaCl (XNaCl = 0.1 and 0.2) acting as heterogeneous nucleation seeds helps overcome the kinetic barrier, leading to the structural growth and crystallization of MgCl2 ⋅ 6H2O. SEM/EDX elemental X-ray mapping showed that the effloresced NaCl-rich particles contain homogeneously crystallized NaCl in the center, surrounded by MgCl2 ⋅ 4H2O. The observation of an aqueous phase over a wider RH range for NaCl–MgCl2 mixture particles indicates their more probable heterogeneous chemistry compared to pure NaCl particles as a nascent SSA surrogate.

Highlights

  • Sea-salt or sea-spray aerosols (SSAs) are produced from waves through bubble bursting and constitute the second most abundant source of natural atmospheric aerosols (25– 50 % of the aerosol mass) after mineral dust particlesPublished by Copernicus Publications on behalf of the European Geosciences Union.D

  • This study systematically describes the full hygroscopic behavior of NaCl– MgCl2 binary aerosol particles at 12 different mixing ratios

  • A dry powder or nebulized pure MgCl2 q 6H2O particles and some NaCl–MgCl2 mixture particles were deposited on a transmission electron microscopy (TEM) grid and/or Al substrates to perform offline SEM/EDX measurements after the hygroscopic measurements by optical microscopy (OM) to avoid charging by the electron beam on the Parafilm-M substrates

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Summary

Introduction

Sea-salt or sea-spray aerosols (SSAs) are produced from waves through bubble bursting and constitute the second most abundant source of natural atmospheric aerosols (25– 50 % of the aerosol mass) after mineral dust particles. The hygroscopic growth factors of ambient or laboratory-generated SSAs plotted as a function of the RH were reported to be different from that of pure NaCl (Tang et al, 1997; Ahn et al, 2010; Schindelholz et al, 2014) This different hygroscopic behavior can affect the cloud-droplet nucleation efficiency. The hygroscopic behavior, physical states/phases, and micro-structures of pure MgCl2 and NaCl–MgCl2 mixture particles (covering 12 mixing ratios with NaCl mole fractions ranging from 0.01 to 0.9) were examined by optical microscopy (OM), in situ Raman micro-spectrometry (RMS), and scanning electron microscopy/energy dispersive X-ray spectrometry (SEM/EDX). This study systematically describes the full hygroscopic behavior of NaCl– MgCl2 binary aerosol particles at 12 different mixing ratios

Preparation of NaCl–MgCl2 mixture particles
Optical microscopy
Results and discussion
Hygroscopic behavior of pure NaCl and MgCl2 particles
Hygroscopic behavior of NaCl–MgCl2 mixture particles
Deliquescence phase diagram of mixed NaCl–MgCl2 particles
Efflorescence phase diagram of mixed NaCl–MgCl2 particles
Spatial distribution of effloresced NaCl–MgCl2 solid particles
Atmospheric implications
Conclusions

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