Experimental sticking coefficients of CO and N_2 on sub-micrometric cosmic grain analogs

C. Stadler, C. Laffon, Ph. Parent
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Abstract

Measuring the sticking coefficient of molecules pertinent to astrochemistry - such as CO - on substrates that mimic interstellar dust grains is crucial for the comprehensive understanding of gas-grain chemical processes. Although astrochemical models assume a sticking coefficient of 1, recent laboratory experiments on H2O and CO2 have revealed significantly lower values when measured on small grain analogs. As the effect of grain size on molecular adsorption has been largely ignored to date, further experiments are needed to determine the accretion rates of species known to freeze out on dust grains. Our aim is to determine the sticking coefficients of CO and N2 on sub-micrometric silicate and carbon grains. By quantifying realistic sticking coefficients on these dust grain analogs, we can improve the accuracy of astrochemists' predictions of molecular abundances as affected by gas-grain interactions. The molecules of interest were added to various substrates at 10 K in an ultra-high vacuum. The amount of adsorbate that stuck to the substrate was quantified using X-ray photoelectron spectroscopy. These quantities were compared to a reference with a sticking coefficient of 1, allowing the deduction of the sticking coefficient for each substrate. The average sticking coefficients of CO and N2 on grain analogs are 0.17 for CO and 0.14 for N2 on olivine powder, and 0.05 for CO and 0.07 on N2 on soot, instead of the presumed 1. This is in line with the low values previously reported for H2O and CO2 These laboratory results indicate that CO and N2 in addition to H2O and CO2 also exhibit a low sticking coefficient on dust grain analogs. It is thus necessary to reconsider the interactions between gaseous species and dust particles as a low-efficiency process. This reduction in accretion and reaction rates has important implications for how we understand astrochemistry.
亚微米宇宙晶粒类似物上 CO 和 N_2 的实验粘滞系数
测量与天体化学有关的分子(如一氧化碳)在模拟星际尘粒的基质上的粘滞系数,对于全面了解气粒化学过程至关重要。尽管天体化学模型假定粘滞系数为 1,但最近对 H2O 和 CO2 进行的实验室实验表明,在小颗粒模拟物上测量的粘滞系数要低得多。由于迄今为止人们在很大程度上忽视了颗粒大小对分子吸附的影响,因此需要进一步的实验来确定已知会冻结在尘埃颗粒上的物种的吸附率。我们的目标是确定 CO 和 N2 在亚微米硅酸盐和碳颗粒上的粘附系数。通过量化这些尘粒类似物上的实际粘滞系数,我们可以提高天体化学专家预测受气体-尘粒相互作用影响的分子丰度的准确性。在 10 K 的超高真空条件下,将相关分子添加到各种基底上。使用 X 射线光电子能谱对粘附在基底上的吸附物数量进行量化。将这些数量与吸附系数为 1 的参照物进行比较,从而推导出每种基底的吸附系数。这些实验室结果表明,除了 H2O 和 CO2 外,CO 和 N2 在尘粒类似物上的粘附系数也很低。因此,有必要将气体物种与尘粒之间的相互作用重新视为一种低效率过程。这种吸积和反应速率的降低对我们如何理解天体化学具有重要影响。
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