Experimental Scattering Matrices of Martian Dust Aerosols with Narrow Particle-size Distributions

Julia Martikainen, Olga Muñoz, Juan Carlos Gómez Martín, Teresa Jardiel, Marco Peiteado, Amador C. Caballero, Santiago Pérez-Hoyos, Agustin Sánchez Lavega, Tim Becker, Gerhard Wurm, Yannick Willame, Ann Carine Vandaele
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Abstract

We present experimental scattering matrices of the JSC Mars-1, MMS-2, and MGS-1 simulants at 488 and 640 nm. The analogs were processed so that narrow size distributions representative of Martian dust aerosols during different dust cycles were obtained. We find that the forward peak of the phase function depends on particle size as it becomes narrower with increasing size, whereas the side- and backscattering directions depend on both composition and size so that increasing size and decreasing absorption produce a flatter curve. The position and maximum of the degree of linear polarization varies based on particle size and composition, and the negative polarization branch is more prominent for wavelength-scale particles diminishing with increasing size. The linear depolarization is strongly affected by size and composition. Finally, we compare sky-brightness curves measured by the Navcam and Hazcam engineering cameras on board the Mars Science Laboratory rover to the measured phase functions. The observations show a narrower peak at the forward direction and a flatter curve toward the side- and backscattering directions with an increasing dust load in the atmosphere, similar to what can be seen for the measured phase functions of the analogs with increasing particle size. In the case of the analogs, the flattening of the curve can be caused by an increase in multiple scattering within a particle by wavelength-scale surface roughness and/or internal inclusions. For the observed sky brightnesses, particle aggregation and multiple scattering among particles in denser dust conditions play a major role.
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具有窄粒径分布的火星尘埃气溶胶的实验散射矩阵
我们展示了 JSC 火星-1、MMS-2 和 MGS-1 模拟物在 488 和 640 纳米波长下的实验散射矩阵。我们对模拟物进行了处理,从而获得了在不同尘埃周期中代表火星尘埃气溶胶的窄粒度分布。我们发现,相位函数的正向峰值取决于颗粒大小,因为它随着颗粒大小的增大而变窄,而侧向和后向散射方向则取决于成分和大小,因此,随着颗粒大小的增大和吸收量的减少,会产生一条较平坦的曲线。线性极化程度的位置和最大值因颗粒大小和成分而异,负极化分支在波长尺度的颗粒中更为突出,随着粒径增大而减弱。线性去极化受粒径和成分的影响很大。最后,我们将火星科学实验室探测器上的 Navcam 和 Hazcam 工程相机测得的天空亮度曲线与测得的相位函数进行了比较。观测结果表明,随着大气中尘埃负荷的增加,前向峰值变窄,侧向和背向散射方向的曲线变平,这与测量到的类似物相位函数随颗粒大小增加而变化的情况类似。就类似物而言,曲线变平的原因可能是波长尺度的表面粗糙度和/或内部夹杂物增加了颗粒内部的多重散射。就观测到的天空亮度而言,颗粒聚集和颗粒间的多重散射在密度较大的尘埃条件下起着主要作用。
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