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Deuterium to hydrogen towards QSO 1009+2956 from a mesoturbulent model

机译:从中湍流模型将氘氢转化为QSO 1009 + 2956

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摘要

We present a new analysis of the deuterium absorption at z = 2.504 towards the quasar Q1009+2956 using the mesoturbulent model which accounts for possible correlations in the large scale velocity field. We obtain a slightly higher deuterium-to-hydrogen ratio D/H = (3.5 - 5.0)*10^{-5} as compared with the recent measurement D/H = (3.3 - 4.5)*10^{-5} (68% C.L.) performed by Burles & Tytler (1998b) using the usual microturbulent approximation which assumes that the velocity field is uncorrelated. Other mesoturbulent calculations of the D-abundances at z = 3.572 towards Q1937--1009 and at z = 0.701 towards Q1718+4807 (the systems showing `low' and possibly `high' D/H values, respectively, in the microturbulent approaches) agree with the present one within the errors of measurements. Thus, the mesoturbulent analysis does not reveal any spatial variations of D/H and supports the standard homogeneous model of big bang nucleosynthesis.
机译:我们使用中湍流模型对z = 2.504时对类星体Q1009 + 2956的氘吸收进行了新的分析,该模型说明了大规模速度场中的可能相关性。与最近的测量值D / H =(3.3-4.5)* 10 ^ {-5}相比,我们获得的氘氢比D / H =(3.5-5.0)* 10 ^ {-5}( Burles&Tytler(1998b)使用通常的微湍流近似法(假设速度场不相关)执行了68%的CL)。到Q1937--1009时z = 3.572处和到Q1718 + 4807时z = 0.701处的D丰度的其他中湍流计算(在微湍流方法中,系统分别显示“低”和“高” D / H值)在测量误差范围内与目前的观点一致。因此,中湍流分析没有揭示D / H的任何空间变化,并且支持了大爆炸核合成的标准同质模型。

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