The study looked at sediments in Huangqihai Lake, Inner Mongolia, to understand changes in sediment dynamics and environment over the past 2000 years. The results showed that the sediments displayed magnetic fabric, with the smallest anisotropy aligned parallel to the bedding plane and the largest anisotropy perpendicular to it. The lake shore had higher magnetic anisotropy, indicating faster flow compared to the lake center. In the western part of the lake, the magnetic properties changed at different depths, suggesting strong depositional events. The sediments could be divided into three stages based on water dynamics and depositional environment stability.