Isotopic hydrological links among precipitation, river water and groundwater in an alpine mountain basin, NE Qinghai–Tibet Plateau in warm seasons

Cao, Shengkui; Cao, Guangchao; Wang, Zhigang; Hou, Yaofang; Wang, Youcai; Kang, Ligang

doi:10.1007/s12665-022-10485-8

Cited by 5 publications

(2 citation statements)

References 56 publications

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“…Existing studies have mainly analyzed the change characteristics of surface water area and the types of disease caused by roadside ponding, but they lack the analysis of influencing factors for surface water on the Qinghai-Tibet Highway, and the severity of diseases caused by roadside ponding is seldom involved [30][31][32][33][34]. Therefore, in order to study the distribution of surface water along the Qinghai-Tibet Highway and analyze the effect of roadside ponding on the subgrade, this paper investigated the surface water in the Qinghai-Tibet Engineering Corridor, conducted on-site surveys and monitored the typical lakes and ponds, and acquired 1059 high-magnitude remote sensing images along the Qinghai-Tibet Highway.…”

Section: Introductionmentioning

confidence: 99%

Characteristics and Influence Rules of Roadside Ponding along the Qinghai–Tibet Highway

Cui,

Zhu,

Liu

et al. 2024

Water

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Due to climate change and seasonal precipitation, water conditions in the Qinghai–Tibet region are a significant factor affecting the stability of subgrades. The accumulation of large amounts of surface water leads to subgrade diseases along the Qinghai–Tibet Highway. Based on remote sensing photos obtained from Google Earth Engine and processing the photos using ENVI 5.6.3 and CAD 2019 software, this paper analyzed the distribution characteristics of surface water and studied the impact of roadside ponding on subgrade diseases. The results showed that the total area of surface water was more than 3.7 million m2, and the surface water was most widely distributed in large river areas such as the Tuotuo River and Buqu River. The subgrade diseases of the Qinghai–Tibet Highway could be categorized into three types: settlement, longitudinal crack, and frost boiling, which accounted for 71.09%, 17.13%, and 11.78% of the total number of subgrade diseases, respectively. Additionally, the ground mean annual temperature was an important factor affecting the distribution of surface water, with the surface water area showing an increasing trend with the increase in ground mean annual temperature, and roadside ponding was most likely to form in the high-temperature extremely unstable permafrost area.

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Section: Introductionmentioning

confidence: 99%

Characteristics and Influence Rules of Roadside Ponding along the Qinghai–Tibet Highway

Cui,

Zhu,

Liu

et al. 2024

Water

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“…Extreme weather disasters come one after another -heavy precipitation, widespread drought, and prolonged high temperatures, which have exacerbated the instability of water resources and the contradiction between supply and demand [5]. As an important point in the water cycle, precipitation is the direct or indirect replenishment source of various water bodies, and its long-term evolution has a decisive influence on regional water resources [6]. The change in precipitation pattern and water cycle process intensifies the complexity of water resources change, resulting in increased uncertainty of precipitation and its spatio-temporal distribution [7].…”

Section: Introductionmentioning

confidence: 99%

The Characteristics of Precipitation During the Flood Seasons in Heilongjiang Province Over the Past 53 Years

Yang,

Yu,

Shi

et al. 2024

OAJRCES

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Based on monthly precipitation data from May to September 1970-2022 from 80 weather stations, methods such as the IDW space interpolation method, Mann-Kendall test, cumulative anomaly method, and wavelet analysis were used to analyze the rainfall trends, periodicity, and mutation characteristics of precipitation during the flood season. The results show: (1) In recent 53 years, the average flood precipitation amount is 459.2 mm, with the most at 784.1 mm (in 2016) and the least at 317.6 mm (in 2007). The flood precipitation has shown a slight trend of increasing at a rate of 2.5 mm/a. (2) The precipitation in flood season reflects obvious intergenerational variation characteristics, mainly in a "W" variation trend, with the average flood precipitation in each decade showing 2000s < 1970s < 1980s < multi-annual average < 1990s < 2010s. (3) The mid part of the province in Yichun, north of Hegang and the middle of Harbin had the highest flood rainfall, the lowest was in the Great Khingan Mountains, the Songnen Plain, and the Sanjiang Plain. The spatial distribution from west to east was characterized by a "lowhigh-low" distribution. (4) There were three time scales, 54, 17, and 6 years, with the first period, the most intense one, being the first primary period. The main cycle of precipitation in flood season is 34a, the sub-cycles are 12a and 4a. (5) The cumulative distance showed a "decline -fluctuate -rise" trend. The flood season precipitation had an abrupt change in 2011 and showed a change from less to more, post-mutation 2012-2022 compared to pre-mutation 1970-2011, the mean increase was 142.5 mm.

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Review: Recent progress on groundwater recharge research in arid and semiarid areas of China

Xie

Dong

et al. 2023

Hydrogeol J

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Isotopic hydrological links among precipitation, river water and groundwater in an alpine mountain basin, NE Qinghai–Tibet Plateau in warm seasons

Cited by 5 publications

References 56 publications

Characteristics and Influence Rules of Roadside Ponding along the Qinghai–Tibet Highway

Characteristics and Influence Rules of Roadside Ponding along the Qinghai–Tibet Highway

The Characteristics of Precipitation During the Flood Seasons in Heilongjiang Province Over the Past 53 Years

Review: Recent progress on groundwater recharge research in arid and semiarid areas of China

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