Jiangli Pang's research while affiliated with Shaanxi Normal University and other places

... Due to intrinsic uncertainty of dating methods, how to precisely constraining the debris flows ages is a key challenge (Wu et al. 2010;Zhao et al. 2015). Because some stratigraphic archives remain unexposed, it is difficult to assess the ages of each debris flow event in the sedimentary sequences (Schneuwly-Bollschweiler et al. 2013;Guo et al. 2016). Hence, selecting the applicable dating material is crucial for obtaining a true depositional age. ...

... Knowing the extent of the lake area can help to understand the lake elements such as the water level and reservoir capacity (high-precision elevation) of the dammed lake, showing that the sediment concentration plays an important role in the outburst of the dammed lake [13][14][15]. In addition, the change of sediment accumulation in the reservoir area of the lake will also affect the movement pattern of the breach flood and the peak flow rate of the breach, so it is important to obtain the change of the area and SSC of the barrier lake in time for the prediction and early warning of the lake breach and for safety prevention [16][17][18][19][20][21]. Since the formation of the Attabad landslide-dammed lake, Chen et al. (2019) calculated the peak burst discharge of the barrier lake and the variation law of flood discharge along the break by using the formula of peak burst discharge based on the field investigation of the Attabad landslide dams and the analysis results of the incoming water and sediment data in the upper reaches of the dammed lake [22]. ...

... Above the Gaoling soil, C2 (a thin platy layer) seems to represent a very short time interval compared with other stratigraphic units, although C2 has not yet been dated. This platy layer could be the result of higher-energy flood deposition, based on its structure and abrupt upper and lower boundaries X. Zhao et al., 2016). Alternatively, C2 is the result of modern, localized construction activity around the site, as the platy layer is expressed in the areas of Yangguanzhai with the most construction work (the northeast corner and north-central portion). It is possible that heavy machinery or construction activities compacted the ground surface and promot ...

... With a mean elevation of 3,400 m, the basin has a relatively flat topography surrounded by high mountains, including the Minshan Mountains, the origin of the studied Black River (Fig. 1b). As a unique area in the Qinghai-Tibet Plateau, the Zoige Basin fosters the world's largest alpine peatland, which was formed by lacustrine deposits of a paleolake that collapsed and drained 37 ka before present (Chen et al., 1999;Nicoll et al., 2013;Zeng et al., 2017;Wang et al., 2023). With a relatively cold alpine climate (Dwc in Köppen Classification), the basin has an annual mean temperature of 0.7 ℃ and annually receives 645 mm of precipitation on average (Li et al., 2014). ...

... Such long-term reconstructions offer sedimentary clues regarding the chronology, magnitude, and frequency of past floods, furnishing a historical lens to better grasp flood hydrology and enhance risk assessment (George et al., 2020). In recent years, numerous palaeoflood investigations have been conducted in the middle and lower reaches of the Yangtze and Yellow rivers (Huang et al., 2010;Liu et al., 2015;Guo et al., 2017Guo et al., , 2018Mao et al., 2016Mao et al., , 2022Zhang et al., 2021b). Sediment grain size variations are a popular tool in these studies to discern past flood events (Huang et al., 2010;Guo et al., 2018;Guan et al., 2022). ...

... In the upper Yellow River, the destruction of the site of Lajia of the Qijia culture has been studied through various palaeoenvironmental means (micromorphology, OSL, paleosol). Around 2200-2000 BC, mudflows caused by rainstorms, flash floods, and earthquakes and the intensive exploitation of the landscape during the Neolithic resulted in the tragedy at Lajia 28, [96][97][98][99][100]. ...

... The data generated from palaeoflood hydrology are of great significance in achieving a better estimate for large events and providing an interpretation of the regional response of the hydrological system to global climatic change at longer time scales (Huang et al., 2010(Huang et al., , 2012a(Huang et al., , 2012bHuang, Li, Pang, Zha, & Zhou, 2012;Huang, Pang, Zha, & Zhou, 2011;Knox, 2000;Luo et al., 2018Luo et al., , 2020. Previous studies have been carried out in the middle and lower reaches of the Yellow River, and its tributaries, such as the Weihe River, the Qinshuihe River, the Luohe River, and so on (Huang et al., 2010(Huang et al., , 2011Huang, Li, et al., 2012;Huang, Pang, et al., 2012a, 2012bLiang, Dong, Yan, & Liu, 2020;Wan, Huang, Ge, & Pang, 2019;Xie, Shi, & Wang, 1998;Yang, Ge, Xie, Zhan, & Li, 2000;Zhang et al., 2019), the main tributaries of the Yangze River, such as the Hanjiang River, the Danjiang River (Guo et al., 2015;Huang et al., 2013;Li, Huang, Zhang, Pang, & Ma, 2020;Liu et al., 2015;Mao et al., 2016;Wang, Huang, Pang, Zha, & Zhou, 2014;Zhou et al., 2016) and the Huaihe River Xie, Wang, & Wang, 2000). However, the investigations have rarely been carried out in the Yellow River source area. ...

... Environmental magnetic analyses have demonstrated that when sediments are fine and the contribution of superparamagnetic (SP) particles is extremely low, χ lf can be used to reflect hydrodynamic changes (Jia et al. 2004;Ji & Xia 2007). The reductive dissolution of granular magnetic minerals would also cause a decrease in χ lf under water-logging conditions (Huang et al. 2011b;Wang et al. 2012;Wan et al. 2019). As a widely used parameter, χ lf is controlled by the type, content, and grain size of magnetic minerals. ...

... Compared with traditional loess landslides, loess mudflows exhibit fluid movement, so a loess mudflow has a greater mobility and a wider accumulation range, leading to greater danger (Leng et al., 2018;Zha et al., 2019). A large number of field investigations have shown that the motion characteristics of loess mudflows mainly include the following aspects. ...

... During the early Holocene (11-6.5 ka), the climate was variable based on the temporal dissimilarity of the paleoclimatic records in the EASM-associated region in China (Zhang et al., 2021) and reconstructed precipitation from Lake Gonghai (GH) in northern China (Chen et al., 2015). The high flooding phase in this period was in response to higher climate fluctuation, and previous studies support these interpretations (Li et al., 2019;Peng et al., 2019). ...