Restoration Lessons from China's Loess Plateau
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Ecosystem Services Changes Between 2000 and 2015 in the Loess Plateau, China: a Response to Ecological Restoration
RESEARCH ARTICLE Ecosystem services changes between 2000 and 2015 in the Loess Plateau, China: A response to ecological restoration Dan Wu1, Changxin Zou1, Wei Cao2*, Tong Xiao3, Guoli Gong4 1 Nanjing Institute of Environmental Sciences, Ministry of Environmental Protection, Nanjing, China, 2 Key Laboratory of Land Surface Pattern and Simulation, Institute of Geographic Sciences and Natural Resources Research, CAS, Beijing, China, 3 Satellite Environment Center, Ministry of Environmental Protection, Beijing, China, 4 Shanxi Academy of Environmental Planning, Taiyuan, China a1111111111 a1111111111 * [email protected] a1111111111 a1111111111 a1111111111 Abstract The Loess Plateau of China is one of the most severe soil and water loss areas in the world. Since 1999, the Grain to Green Program (GTGP) has been implemented in the region. This OPEN ACCESS study aimed to analyze spatial and temporal variations of ecosystem services from 2000 to Citation: Wu D, Zou C, Cao W, Xiao T, Gong G 2015 to assess the effects of the GTGP, including carbon sequestration, water regulation, (2019) Ecosystem services changes between 2000 soil conservation and sand fixation. During the study period, the area of forest land and and 2015 in the Loess Plateau, China: A response grassland significantly expanded, while the area of farmland decreased sharply. Ecosystem to ecological restoration. PLoS ONE 14(1): services showed an overall improvement with localized deterioration. Carbon sequestration, e0209483. https://doi.org/10.1371/journal. pone.0209483 water regulation and soil conservation increased substantially. Sand fixation showed a decreasing trend mainly because of decreased wind speeds. There were synergies Editor: Debjani Sihi, Oak Ridge National Laboratory, UNITED STATES between carbon sequestration and water regulation, and tradeoffs between soil conserva- tion and sand fixation. -
Optical and Physical Characteristics of the Lowest Aerosol Layers Over the Yellow River Basin
atmosphere Article Optical and Physical Characteristics of the Lowest Aerosol Layers over the Yellow River Basin Miao Zhang 1,*, Jing Liu 2, Muhammad Bilal 3,* , Chun Zhang 1, Feifei Zhao 1, Xiaoyan Xie 4,5 and Khaled Mohamed Khedher 6,7 1 School of Environmental Science and Tourism, Nanyang Normal University, Wolong Road No.1638, Nan Yang 473061, China; [email protected] (C.Z.); zff@nynu.edu.cn (F.Z.) 2 Lingnan College, Sun Yat-sen University, Guangzhou 510275, China; [email protected] 3 School of Marine Sciences, Nanjing University of Information Science & Technology, Nanjing 2100444, China 4 South China Sea Fisheries Research Institute, Chinese Academy of Fishery Sciences, Guangzhou 510300, China; [email protected] 5 College of Marine Science, Shanghai Ocean University, Shanghai 201306, China 6 Department of Civil Engineering, College of Engineering, King Khalid University, Abha 61421, Saudi Arabia; [email protected] 7 Department of Civil Engineering, Institut Superieur des Etudes Technologiques, Campus Universitaire Mrezgua, Nabeul 8000, Tunisia * Correspondence: [email protected] (M.Z.); [email protected] (M.B.) Received: 17 September 2019; Accepted: 19 October 2019; Published: 22 October 2019 Abstract: Studying the presence of aerosols in different atmospheric layers helps researchers understand their impacts on climate change, air quality, and human health. Therefore, in the present study, the optical and physical properties of aerosol layers over the Yellow River Basin (YERB) were investigated using the CALIPSO Level 2 aerosol layer products from January 2007 to December 2014. The Yellow River Basin was divided into three sub-regions i.e., YERB1 (the plain region downstream of the YERB), YERB2 (the Loess Plateau region in the middle reaches of the YERB), and YERB3 (the mountainous terrain in the upper reaches of the YERB). -
Landslides on the Loess Plateau of China: a Latest Statistics Together with a Close Look
Landslides on the Loess Plateau of China: a latest statistics together with a close look Xiang-Zhou Xu, Wen-Zhao Guo, Ya- Kun Liu, Jian-Zhong Ma, Wen-Long Wang, Hong-Wu Zhang & Hang Gao Natural Hazards Journal of the International Society for the Prevention and Mitigation of Natural Hazards ISSN 0921-030X Volume 86 Number 3 Nat Hazards (2017) 86:1393-1403 DOI 10.1007/s11069-016-2738-6 1 23 Your article is protected by copyright and all rights are held exclusively by Springer Science +Business Media Dordrecht. This e-offprint is for personal use only and shall not be self- archived in electronic repositories. If you wish to self-archive your article, please use the accepted manuscript version for posting on your own website. You may further deposit the accepted manuscript version in any repository, provided it is only made publicly available 12 months after official publication or later and provided acknowledgement is given to the original source of publication and a link is inserted to the published article on Springer's website. The link must be accompanied by the following text: "The final publication is available at link.springer.com”. 1 23 Author's personal copy Nat Hazards (2017) 86:1393–1403 DOI 10.1007/s11069-016-2738-6 SHORT COMMUNICATION Landslides on the Loess Plateau of China: a latest statistics together with a close look 1,2 2 2 Xiang-Zhou Xu • Wen-Zhao Guo • Ya-Kun Liu • 1 1 3 Jian-Zhong Ma • Wen-Long Wang • Hong-Wu Zhang • Hang Gao2 Received: 16 December 2016 / Accepted: 26 December 2016 / Published online: 3 January 2017 Ó Springer Science+Business Media Dordrecht 2017 Abstract Landslide plays an important role in landscape evolution, delivers huge amounts of sediment to rivers and seriously affects the structure and function of ecosystems and society. -
A Study of Unstable Slopes in Permafrost Areas: Alaskan Case Studies Used As a Training Tool
A Study of Unstable Slopes in Permafrost Areas: Alaskan Case Studies Used as a Training Tool Item Type Report Authors Darrow, Margaret M.; Huang, Scott L.; Obermiller, Kyle Publisher Alaska University Transportation Center Download date 26/09/2021 04:55:55 Link to Item http://hdl.handle.net/11122/7546 A Study of Unstable Slopes in Permafrost Areas: Alaskan Case Studies Used as a Training Tool Final Report December 2011 Prepared by PI: Margaret M. Darrow, Ph.D. Co-PI: Scott L. Huang, Ph.D. Co-author: Kyle Obermiller Institute of Northern Engineering for Alaska University Transportation Center REPORT CONTENTS TABLE OF CONTENTS 1.0 INTRODUCTION ................................................................................................................ 1 2.0 REVIEW OF UNSTABLE SOIL SLOPES IN PERMAFROST AREAS ............................... 1 3.0 THE NELCHINA SLIDE ..................................................................................................... 2 4.0 THE RICH113 SLIDE ......................................................................................................... 5 5.0 THE CHITINA DUMP SLIDE .............................................................................................. 6 6.0 SUMMARY ......................................................................................................................... 9 7.0 REFERENCES ................................................................................................................. 10 i A STUDY OF UNSTABLE SLOPES IN PERMAFROST AREAS 1.0 INTRODUCTION -
The Distribution of Silty Soils in the Grayling Fingers Region of Michigan: Evidence for Loess Deposition Onto Frozen Ground
Geomorphology 102 (2008) 287–296 Contents lists available at ScienceDirect Geomorphology journal homepage: www.elsevier.com/locate/geomorph The distribution of silty soils in the Grayling Fingers region of Michigan: Evidence for loess deposition onto frozen ground Randall J. Schaetzl ⁎ Department of Geography, 128 Geography Building, Michigan State University, East Lansing, MI, 48824-1117, USA ARTICLE INFO ABSTRACT Article history: This paper presents textural, geochemical, mineralogical, soils, and geomorphic data on the sediments of the Received 12 September 2007 Grayling Fingers region of northern Lower Michigan. The Fingers are mainly comprised of glaciofluvial Received in revised form 25 March 2008 sediment, capped by sandy till. The focus of this research is a thin silty cap that overlies the till and outwash; Accepted 26 March 2008 data presented here suggest that it is local-source loess, derived from the Port Huron outwash plain and its Available online 10 April 2008 down-river extension, the Mainstee River valley. The silt is geochemically and texturally unlike the glacial fl Keywords: sediments that underlie it and is located only on the attest parts of the Finger uplands and in the bottoms of Glacial geomorphology upland, dry kettles. On sloping sites, the silty cap is absent. The silt was probably deposited on the Fingers Loess during the Port Huron meltwater event; a loess deposit roughly 90 km down the Manistee River valley has a Permafrost comparable origin. Data suggest that the loess was only able to persist on upland surfaces that were either Kettles closed depressions (currently, dry kettles) or flat because of erosion during and after loess deposition. -
Mysterious Carvings and Evidence of Human Sacrifice Uncovered in Ancient City
Mysterious carvings and evidence of human sacrifice uncovered in ancient city Discoveries at the sprawling site have archaeologists rethinking the roots of Chinese civilization. By Brook Larmer PUBLISHED August 6, 2020 The stones didn’t give up their secrets easily. For decades, villagers in the dust-blown hills of China’s Loess Plateau believed that the crumbling rock walls near their homes were part of the Great Wall. It made sense. Remnants of the ancient barrier zigzag through this arid region inside the northern loop of the Yellow River, marking the frontier of Chinese rule stretching back more than 2,000 years. But one detail was curiously out of place: Locals, and then looters, began finding in the rubble pieces of jade, some fashioned into discs and blades and scepters. Jade is not indigenous to this northernmost part of Shaanxi Province— the nearest source is almost a thousand miles away—and it was not a known feature of the Great Wall. Why was it Join archaeologists as they search for clues to the mysterious fate of “China’s Pompeii” in a new three-part series. Ancient China from Above premiers in the U.S. Tuesday August 11 at 10/9c on National Geographic. For all other countries check local listings. When a team of Chinese archaeologists came to investigate the conundrum several years ago, they began to unearth something wondrous and puzzling. The stones were not part of the Great Wall but the ruins of a magnificent fortress city. The ongoing dig has revealed more than six miles of protective walls surrounding a 230-foot-high pyramid and an inner sanctum with painted murals, jade artifacts—and gruesome evidence of human sacrifice. -
China's Special Poor Areas and Their Geographical Conditions
sustainability Article China’s Special Poor Areas and Their Geographical Conditions Xin Xu 1,2, Chengjin Wang 1,2,*, Shiping Ma 1,2 and Wenzhong Zhang 1,2 1 Institute of Geographic Sciences and Natural Resources Research, Chinese Academy of Sciences, Beijing 100101, China; [email protected] (X.X.); [email protected] (S.M.); [email protected] (W.Z.) 2 College of Resources and Environment, University of Chinese Academy of Sciences, Beijing 100049, China * Correspondence: [email protected] Abstract: Special functional areas and poor areas tend to spatially overlap, and poverty is a common feature of both. Special poor areas, taken as a kind of “policy space,” have attracted the interest of researchers and policymakers around the world. This study proposes a basic concept of special poor areas and uses this concept to develop a method to identify them. Poor counties in China are taken as the basic research unit and overlaps in spatial attributes including old revolutionary bases, borders, ecological degradation, and ethnic minorities, are used to identify special poor areas. The authors then analyze their basic quantitative structure and pattern of distribution to determine the geographical bases’ formation and development. The results show that 304 counties in China, covering a vast territory of 12 contiguous areas that contain a small population, are lagging behind the rest of the country. These areas are characterized by rich energy and resource endowments, important ecological functions, special historical status, and concentrated poverty. They are considered “special poor” for geographical reasons such as a relatively harsh natural geographical environment, remote location, deteriorating ecological environment, and an inadequate infrastructure network and public service system. -
Global Cooling and Enhanced Eocene Asian Mid-Latitude Interior Aridity
ARTICLE DOI: 10.1038/s41467-018-05415-x OPEN Global cooling and enhanced Eocene Asian mid-latitude interior aridity J.X. Li1,2, L.P. Yue2,3, A.P. Roberts4, A.M. Hirt 5, F. Pan1,2, Lin Guo1,Y.Xu1, R.G. Xi1, Lei Guo1, X.K. Qiang3, C.C. Gai6,7, Z.X. Jiang4,7,8, Z.M. Sun9 & Q.S. Liu 10 Tibetan Plateau uplift has been suggested as the main driving force for mid-latitude Asian inland aridity (AIA) and for deposition of thick aeolian sequences in northern China since the 1234567890():,; Miocene. However, the relationship between earlier AIA and Tibetan Plateau mountain building is uncertain because of a lack of corresponding thick aeolian sequences with accurate age constraints. We here present results for a continuous aeolian sequence that spans the interval from >51 to 39 Ma from the eastern Xorkol Basin, Altun Shan, northeastern Tibetan Plateau. The basal age of the studied sequence postdates initial uplift of the Tibetan Plateau by several million years. Our results indicate that the local palaeoclimate was tele- connected strongly to the overall global cooling pattern, so that local enhanced aridification recorded by the studied aeolian sequence is dominantly a response to global climatic forcing rather than plateau uplift. 1 Research Center for Orogenic Geology, Xi’an Center of Geological Survey, China Geological Survey, Xi’an 710054, China. 2 State Key Laboratory for Continental Dynamics, Department of Geology, Northwest University, Xi’an 710127, China. 3 State Key Laboratory of Loess and Quaternary Geology, Institute of Earth Environment, Chinese Academy of Sciences, Xi’an 710061, China. -
Italy and China Sharing Best Practices on the Sustainable Development of Small Underground Settlements
heritage Article Italy and China Sharing Best Practices on the Sustainable Development of Small Underground Settlements Laura Genovese 1,†, Roberta Varriale 2,†, Loredana Luvidi 3,*,† and Fabio Fratini 4,† 1 CNR—Institute for the Conservation and the Valorization of Cultural Heritage, 20125 Milan, Italy; [email protected] 2 CNR—Institute of Studies on Mediterranean Societies, 80134 Naples, Italy; [email protected] 3 CNR—Institute for the Conservation and the Valorization of Cultural Heritage, 00015 Monterotondo St., Italy 4 CNR—Institute for the Conservation and the Valorization of Cultural Heritage, 50019 Sesto Fiorentino, Italy; [email protected] * Correspondence: [email protected]; Tel.: +39-06-90672887 † These authors contributed equally to this work. Received: 28 December 2018; Accepted: 5 March 2019; Published: 8 March 2019 Abstract: Both Southern Italy and Central China feature historic rural settlements characterized by underground constructions with residential and service functions. Many of these areas are currently tackling economic, social and environmental problems, resulting in unemployment, disengagement, depopulation, marginalization or loss of cultural and biological diversity. Both in Europe and in China, policies for rural development address three core areas of intervention: agricultural competitiveness, environmental protection and the promotion of rural amenities through strengthening and diversifying the economic base of rural communities. The challenge is to create innovative pathways for regeneration based on raising awareness to inspire local rural communities to develop alternative actions to reduce poverty while preserving the unique aspects of their local environment and culture. In this view, cultural heritage can be a catalyst for the sustainable growth of the rural community. -
S41598-021-96384-7.Pdf
www.nature.com/scientificreports OPEN A mechanical insight into the triggering mechanism of frequently occurred landslides along the contact between loess and red clay Baoqin Lian1, Xingang Wang1*, Kai Liu1, Sheng Hu2 & Xiao Feng3 The triggering mechanism and movement evolution of loess-red clay landslides, which occurred frequently along the contact between the loess and red clay on the Loess Plateau, are closely related to the mechanical properties of the contact surface. This work presents an experimental investigation on loess, clay and loess-red clay interlaminar (LRCI) samples obtained from a typical loess-red clay landslide in northern part of Shaanxi province of China, using a series of ring shear tests, microscopic observation and scanning electron microscopy tests, in an attempt to explore the mechanical behavior of loess, clay and LRCI samples with variation in moisture content, normal stress and shear rate. The results revealed that for all specimens, both the peak shear strength τp and the residual shear strength τr decreased with increasing moisture content, among which, moisture content has the greatest infuence on the τp and τr of red clay, followed by the LRCI specimen, and the loess specimen is least afected by moisture content. Meanwhile, exponential functions describing the correlations between shear strength and moisture content of LRCI, red clay and loess specimens were proposed. Furthermore, the macroscopic morphological characteristics and the microstructure of shear surface obtained from the LRCI specimens showed that a localized water accumulation was built up within the shear surface as the water content increases to some extent, and a high degree of liquefaction developed within shear surface when the moisture content reached to the saturate degree. -
The Spreading of Christianity and the Introduction of Modern Architecture in Shannxi, China (1840-1949)
Escuela Técnica Superior de Arquitectura de Madrid Programa de doctorado en Concervación y Restauración del Patrimonio Architectónico The Spreading of Christianity and the introduction of Modern Architecture in Shannxi, China (1840-1949) Christian churches and traditional Chinese architecture Author: Shan HUANG (Architect) Director: Antonio LOPERA (Doctor, Arquitecto) 2014 Tribunal nombrado por el Magfco. y Excmo. Sr. Rector de la Universidad Politécnica de Madrid, el día de de 20 . Presidente: Vocal: Vocal: Vocal: Secretario: Suplente: Suplente: Realizado el acto de defensa y lectura de la Tesis el día de de 20 en la Escuela Técnica Superior de Arquitectura de Madrid. Calificación:………………………………. El PRESIDENTE LOS VOCALES EL SECRETARIO Index Index Abstract Resumen Introduction General Background........................................................................................... 1 A) Definition of the Concepts ................................................................ 3 B) Research Background........................................................................ 4 C) Significance and Objects of the Study .......................................... 6 D) Research Methodology ...................................................................... 8 CHAPTER 1 Introduction to Chinese traditional architecture 1.1 The concept of traditional Chinese architecture ......................... 13 1.2 Main characteristics of the traditional Chinese architecture .... 14 1.2.1 Wood was used as the main construction materials ........ 14 1.2.2 -
Summarization and Comparison of Engineering Properties of Loess in the United States
Summarization and Comparison of Engineering Properties of Loess in the United States J. B. SHEELER, Associate Professor of Civil Engineering, Iowa State University •LARGE deposits of loess are found in many parts of the United States, but published values of the engineering properties of loess are relatively scarce. The data in this paper were gathered to indicate similarities and compare the properties of loess from one area with another. Loess is composed primarily of rather loosely arranged angular grains of sand, silt, and clay. Silt is usually the dominant size. Calcite is also generally present in amounts ranging from zero to more than 10 percent of the total soil.. The aeolian hypothesis of loess deposition is compatible with the physical charac teristics of undisturbed loess masses. This hypothesis states that fine-grained ma terial was transported, sorted, and redeposited by wind action and thus became loess. During deposition, moisture and clay minerals are believed responsible for cementing the coarser grains together to form a loose structure. The loess is therefore subject to loss of shear strength due to water softening the clay bonds and to severe consolida tion caused by a combination of loading and moisture. Loess is usually thought of as an aeolian material that was deposited thousands of years ago and has remained in place since the time of deposition. Loess that has been eroded and redeposited is often referred to as redeposited loess, reworked loess or more simply as a silt deposit. This implies that the word loess indicates an aeolian soil, undisturbed since deposition. Certain engineering properties of loess, such as shear strength, are quite drastically changed by erosion and redeposition.