论文标题
拉格朗日结构形成理论相对论宇宙学。 vi。与Szekeres精确解决方案进行比较
Lagrangian theory of structure formation in relativistic cosmology. VI. Comparison with Szekeres exact solutions
论文作者
论文摘要
我们研究了Szekeres模型与相对论Lagrangian扰动方案之间的关系,特别是相对论Zel'Dovich近似(RZA)。我们表明,当Szekeres溶液的第二类解决方案完全包含在RZA内,而后者仅限于具有时空的流动式叶片的无缘尘来源。在这种情况下,该解决方案由变形场的第一个主要标量不变性,证明了与一类无需对称的牛顿三维解决方案的直接连接。对于第二类,通过整体约束表达了宇宙倒流消失的必要条件。没有反应的域可以平滑匹配,形成晶格模型,在给定的均匀性规模上,精确的偏差为平均值,同质和各向同性背景被恢复为模型的平均特性。尽管与第一类Szekeres解决方案的联系并不直接,但此类允许根据非电向流体线的空间叠加来解释,其中每条世界线都独立和RZA模型方程式下来,但具有不同的相关“本地背景”。这指出了将拉格朗日扰动方案推广到在不断发展的背景上(包括全球宇宙反应)上结构形成模型的可能性。
We examine the relation between the Szekeres models and relativistic Lagrangian perturbation schemes, in particular the Relativistic Zel'dovich Approximation (RZA). We show that the second class of the Szekeres solutions is exactly contained within the RZA when the latter is restricted to an irrotational dust source with a flow-orthogonal foliation of spacetime. In such a case, the solution is governed by the first principal scalar invariant of the deformation field, proving a direct connection with a class of Newtonian three-dimensional solutions without symmetry. For the second class, a necessary and sufficient condition for the vanishing of cosmological backreaction on a scale of homogeneity is expressed through integral constraints. Domains with no backreaction can be smoothly matched, forming a lattice model, where exact deviations average out at a given scale of homogeneity, and the homogeneous and isotropic background is recovered as an average property of the model. Although the connection with the first class of Szekeres solutions is not straightforward, this class allows for the interpretation in terms of a spatial superposition of nonintersecting fluid lines, where each world line evolves independently and under the RZA model equations, but with different associated `local backgrounds'. This points to the possibility of generalizing the Lagrangian perturbation schemes to structure formation models on evolving backgrounds, including global cosmological backreaction.