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125 results on '"Niu, Hewen"'

9. A Study of Chemical Processes of Nitrate in Atmospheric Aerosol and Snow Based on Stable Isotopes.

Author

Chen, Mengxue, Niu, Hewen, and Xiang, Yankun

Subjects
*CHEMICAL processes, *ATMOSPHERIC aerosols, *STABLE isotopes, *SNOW chemistry, *POLLUTANTS
Abstract

Nitrate (NO3−) is a prominent atmospheric pollutant and a key chemical constituent of snow and ice, which plays a crucial role in the atmosphere and significantly impacts regional climate and environment conditions through a series of complex chemical processes. By summarizing the recent research progress on the nitrate chemical process (particularly on the isotopic measurements of NO3− (δ15N, Δ17O and δ18O)) in atmosphere and glacier snow, this study mainly investigated the chemical compositions and chemical processes, formation pathways, and photochemical reactions of nitrate in snow and atmosphere. Our results identified that the main ways of atmospheric nitrate formation are the hydrolysis of N2O5 and the reaction of ·OH with NO2; the spatial distribution of Δ17O and δ18O values of atmospheric nitrate have a significant latitudinal trend between 30° N–60° N; the study of stable isotopes (δ15N and δ18O) and the oxygen isotope anomaly (Δ17O) of nitrate have mainly been carried out over the densely populated and coastal mega cities; there exist significant gaps in the study of chemistry processes of nitrate in snow and ice and the air–snow interfaces across glaciated regions. This study provides a basic reference for more robust observations and research of nitrate in glacier areas in the future. [ABSTRACT FROM AUTHOR]

Published
2024
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20. Black carbon and organic carbon dataset over the Third Pole

Author

Kang, Shichang, primary, Zhang, Yulan, additional, Chen, Pengfei, additional, Guo, Junming, additional, Zhang, Qianggong, additional, Cong, Zhiyuan, additional, Kaspari, Susan, additional, Tripathee, Lekhendra, additional, Gao, Tanguang, additional, Niu, Hewen, additional, Zhong, Xinyue, additional, Chen, Xintong, additional, Hu, Zhaofu, additional, Li, Xiaofei, additional, Li, Yang, additional, Neupane, Bigyan, additional, Yan, Fangping, additional, Rupakheti, Dipesh, additional, Gul, Chaman, additional, Zhang, Wei, additional, Wu, Guangming, additional, Yang, Ling, additional, Wang, Zhaoqing, additional, and Li, Chaoliu, additional

Published
2022
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21. Black carbon and dust in the Third Pole glaciers: Revaluated concentrations, mass absorption cross-sections and contributions to glacier ablation

Author

Li, Yang, primary, Kang, Shichang, additional, Zhang, Xuelei, additional, Chen, Jizu, additional, Schmale, Julia, additional, Li, Xiaofei, additional, Zhang, Yulan, additional, Niu, Hewen, additional, Li, Zhongqin, additional, Qin, Xiang, additional, He, Xiaobo, additional, Yang, Wei, additional, Zhang, Guoshuai, additional, Wang, Shijin, additional, Shao, Lili, additional, and Tian, Lide, additional

Published
2021
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25. APCC Data Report I: Black carbon and organic carbon dataset from atmosphere, glaciers, snow cover, precipitation, and lake sediment cores over the Third Pole

Author

Kang, Shichang, primary, Zhang, Yulan, additional, Chen, Pengfei, additional, Guo, Junming, additional, Zhang, Qianggong, additional, Cong, Zhiyuan, additional, Kaspari, Susan, additional, Tripathee, Lekhendra, additional, Gao, Tanguang, additional, Niu, Hewen, additional, Zhong, Xinyue, additional, Chen, Xintong, additional, Hu, Zhaofu, additional, Li, Xiaofei, additional, Li, Yang, additional, Neupane, Bigyan, additional, Yan, Fangping, additional, Rupakheti, Dipesh, additional, Gul, Chaman, additional, Zhang, Wei, additional, Wu, Guangming, additional, Yang, Ling, additional, Wang, Zhaoqing, additional, and Li, Chaoliu, additional

Published
2021
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30. Carbonaceous aerosol characteristics on the Third Pole: A primary study based on the Atmospheric Pollution and Cryospheric Change (APCC) network

Author

Chen, Pengfei, primary, Kang, Shichang, additional, Li, Chaoliu, additional, Zhang, Qianggong, additional, Guo, Junming, additional, Tripathee, Lekhendra, additional, Zhang, Yulan, additional, Li, Gang, additional, Gul, Chaman, additional, Cong, Zhiyuan, additional, Wan, Xin, additional, Niu, Hewen, additional, Panday, Arnico K., additional, Rupakheti, Maheswar, additional, and Ji, Zhenming, additional

Published
2019
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36. Levels and spatial distributions of levoglucosan and dissolved organic carbon in snowpits over the Tibetan Plateau glaciers

Author

Li, Quanlian, primary, Wang, Ninglian, additional, Barbante, Carlo, additional, Kang, Shichang, additional, Yao, Ping, additional, Wan, Xin, additional, Barbaro, Elena, additional, del Carmen Villoslada Hidalgo, Maria, additional, Gambaro, Andrea, additional, Li, Chaoliu, additional, Niu, Hewen, additional, Dong, Zhiwen, additional, and Wu, Xiaobo, additional

Published
2018
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40. Vegetation succession on Baishui No.1 glacier foreland, Mt. Yulong

Author

朱国锋 Zhu Guofeng, 赵勇 Zhao Yong, 张涛 Zhang Tao, 常丽 Chang Li, 牛贺文 Niu Hewen, 何元庆 He Yuanqing, 蒲焘 Pu Tao, 杨太保 Yang Taibao, and 杜建括 Du Jiankuo

Subjects
Carex, geography.geographical_feature_category, Ecology, biology, ved/biology, Chronosequence, ved/biology.organism_classification_rank.species, Glacier, Ecological succession, biology.organism_classification, Shrub, Geography, Moraine, Glacier foreland, Ecology, Evolution, Behavior and Systematics, Terminal moraine
Abstract

A chronosequence study(substituting space for time) was conducted following the retreat of alpine glaciers since the Little Ice Age.The study area is Baishui No.1 Glacier,Mt.Yulong in Lijiang City,Yunnan Province of China.It is the biggest glacier on Yulong Snow Mountain.It has an area of 1.32 km2,the altitude of the equilibrium line is around 4850 m.After the greater advancement of Baishui No.1 Glacier in Little Ice Age,the glacier had began to retreat,and form a large newly-exposed area.This area was divided into five successional seres: SUC1 ≈ 0—9 years;SUC2 ≈ 5—14 years;SUC5 ≈ 200—400 years.They were bounded by dated moraines deposited in 2002,1997,and 17th and 19th centuries.but the age of the two seres(SUC3 and SUC4) is unknow,they were located at an elevation of 4000 m and 3900 m.Then a successional sequence is formed by SUC1 to SUC5.Only a single site was chosen to represent each successional sere.At each sere ten 0.25 m2 quadrats were chosen,we recorded percent cover,height and abundance of each herbaceous species.In SUC4 and SUC5,three 16 m2 and two 100 m2 quadrats were chosen to record height and abundance of bushes and trees respectively. By employing field investigation,factor analysis methods,this study mainly focuses on the communities composition and its number characteristics within different successional times,as well as the variations of vegetation types and the estimation to the age of the terminal moraine in the Little Ice Age.Among the investigated 55 plots,there are 91 types of plants,and about 63 species have been identified from it yet.They belong to 28 families and 46 genera,including arbor,shrub and herb three life forms plants,and most of species are dicotyledon,The number characteristics analysis for different succession stages reveals the communities composition and substitution regulation.Community composition is as follows: In the first successional sere,there are Cerastium caespitosum,Meconopsis horridula and Juncus brachystigma three communities,the dominant species is Cerastium caespitosum;In SUC2,two communities are Polygonum macrophyllum and Carex capilliformis,the former is the dominant;Cerastium caespitosum,Carex capilliformis,Carex crebra and Pedicularis sp.are the main communities in SUC3,and the dominant species is Cerastium caespitosum;Three communities are formed by Carex capilliformis,Carex crebra and Delphinium sp.,and the first one is the dominant in SUC4;Carex crebra,Ligusticum rechingerana and carex kansuensis are the primary communities in the last successional sere.Carex crebra is the dominant species.At the terminal of Baishui No.1 Glacier,the vegetation succession experienced the stages of bare land—herbaceous—shrub—macrophanerophytes.From the perspective of ecological niche,the appearance of this succession process is due to the different ecological niches and their different suitability.The dominant species generally with the wide ecological niche and strong suitability,and can appear in many succession stages.Therefore,the succession toward the orientations of continuing differentiation of ecological niches,and each species try to take advantage of various resources.The species substitution processes often occur under the conditions of intense intraspecies and interspecies crossing competitions.In addition,based on the comprehensively analyses to the geographical characteristics,meteorological features of Mt.Gongga and Mt.Yulong,as well as the vegetation succession process,combing tree-ring materials of Mt.Yulong region,we estimated that the age of terminal moraine is about 170—250 years.

Published
2013

43. Water-soluble elements in snow and ice on Mt. Yulong

Author

Niu, Hewen, primary, Kang, Shichang, additional, Shi, Xiaofei, additional, He, Yuanqing, additional, Lu, Xixi, additional, Shi, Xiaoyi, additional, Paudyal, Rukumesh, additional, Du, Jiankuo, additional, Wang, Shijin, additional, Du, Jun, additional, and Chen, Jizu, additional

Published
2017
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47. Vegetation succession on Baishui No.1 glacier foreland, Mt. Yulong

Author

CHANG Li, 常丽, primary, HE Yuanqing, 何元庆, additional, YANG Taibao, 杨太保, additional, ZHAO Yong, 赵勇, additional, ZHU Guofeng, 朱国锋, additional, NIU Hewen, 牛贺文, additional, ZHANG Tao, 张涛, additional, DU Jiankuo, 杜建括, additional, and PU Tao, 蒲焘, additional

Published
2013
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