Bibliografías temáticas / Yellow River (China)

Literatura académica sobre el tema "Yellow River (China)"

Autor: Grafiati

Publicado: 4 de junio de 2021

Última modificación: 1 de febrero de 2022

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Artículos de revistas sobre el tema "Yellow River (China)":

Lawler, A. "Beyond the Yellow River: How China Became China". Science 325, n.º 5943 (20 de agosto de 2009): 930–35. http://dx.doi.org/10.1126/science.325_930.

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Runhua, Huang. "Arsenic in the Yellow river, China". Earth Surface Processes and Landforms 11, n.º 2 (marzo de 1986): 117–22. http://dx.doi.org/10.1002/esp.3290110202.

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Zuo, Qiting, Minghui Hao, Zhizhuo Zhang y Long Jiang. "Assessment of the Happy River Index as an Integrated Index of River Health and Human Well-Being: A Case Study of the Yellow River, China". Water 12, n.º 11 (1 de noviembre de 2020): 3064. http://dx.doi.org/10.3390/w12113064.

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Acceleration urbanization and industrialization has resulted in challenges such as river ecosystem degradation and water scarcity that have hindered sustainable development in China. Healthy rivers provide ecosystem services that improve human well-being. The Happy River Index (HRI) integrates trends in river health and human well-being. This study aimed to establish an HRI assessment framework. The assessment framework was applied to the Yellow River, China at three spatial scales in which the analytic hierarchy process (AHP)-entropy weight and single index quantification-multiple indices syntheses-poly-criteria integration (SMI-P) methods were utilized. Limiting factors were diagnosed by the obstacle degree model and approaches to improve the HRI in regions along the Yellow River are suggested. The results showed that: (1) the overall HRI of the Yellow River was relatively low, with some differences among different regions; (2) the HRI for the upper, middle, and lower reaches of the Yellow River showed a decreasing trend from 0.77 to 0.65; (3) Sichuan had the highest HRI at the regional scale, followed by Gansu and Qinghai, whereas Inner Mongolia had the lowest; (4) scarcity of water resources and the fragility of the ecological environment were the two dominant factors restricting the improvement of the HRI in regions along the Yellow River. The results of this study can provide a valuable reference for protection of river health and improvement of human well-being in China.

Liu, Jianrong, Xiangfang Song, Zhimin Wang, Lihu Yang, Zhenyu Sun y Wenjia Wang. "Variations of carbon transport in the Yellow River, China". Hydrology Research 46, n.º 5 (16 de agosto de 2014): 746–62. http://dx.doi.org/10.2166/nh.2014.077.

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The Yellow River is the second largest river in China. Carbon transport by the Yellow River has significant influence on riverine carbon cycles in Asia. In order to monitor seasonal and spatial variations of carbon concentrations and to estimate carbon exports, water and suspended solids were sampled every 10 days at three representative stations (Qingtongxia, Tongguan, and Luokou) along the mainstream of the Yellow River. Results showed that riverine carbon was mainly in dissolved form, except during flood period and water and sediment regulation (WSR) scheme, when particulate organic carbon (POC) dominated. Concentration of dissolved inorganic carbon was mostly 5 to 10 times higher than that of dissolved organic carbon (DOC). DOC was mainly related to a natural process (leaching effect) in the upstream and anthropogenic activities in the midstream (domestic sewage and fertilizer application) and downstream (industrial wastewater). POC was connected with high suspended solids. Annually carbon delivered to the Bohai Sea was 1.34 × 1012 g/yr, accounting for 0.15% of the global total riverine carbon flux. Mean DOC exported accounted for 0.12% of the Asian rivers' DOC flux. WSR played an important role in the carbon transport, which accounted for 1/5 to 1/3 of the corresponding annual fluxes.

Dongguang, Wen, Zhang Fawang, Zhang Eryong, Gao Cunrong y Zhantao Han. "Outline of the Yellow River basin, China". BULLETIN OF THE GEOLOGICAL SURVEY OF JAPAN 60, n.º 1-2 (2008): 9–18. http://dx.doi.org/10.9795/bullgsj.60.9.

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Shucheng, Wang. "Water resources management of the Yellow River and sustainable water development in China". Water Policy 5, n.º 4 (1 de agosto de 2003): 305–12. http://dx.doi.org/10.2166/wp.2003.0018.

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China is a country frequently hit by floods and droughts. Managing water resources and minimizing the losses caused by water disasters has always been among the most important issues faced by the Chinese government in governing the state. In recent years, to tackle the water problems in China and to meet the requirement of sustainable economic and social development, we have actively pursued sustainable water development. Thinking about water management has thus been greatly modified and remarkable achievements have been made accordingly. The Yellow River, known as the Mother River of China, is the cradle of Chinese civilization, whose problems can represent that of most Chinese rivers. Citing the Yellow River management in recent years as an example, this paper elaborates the strategy of sustainable water development in China.

Storozum, Michael J., Duowen Mo, Hui Wang, Xiaolin Ren, Yifei Zhang y Tristram R. Kidder. "Anthropogenic origins of a late Holocene, basin-wide unconformity in the middle reaches of the Yellow River, the Luoyang Basin, Henan Province, China". Quaternary Research 87, n.º 3 (6 de abril de 2017): 423–41. http://dx.doi.org/10.1017/qua.2017.10.

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AbstractWe evaluate the relative importance of climate change, fluvial dynamics, and anthropogenic environmental modification in forming the Holocene sedimentary record of the Luoyang Basin, a tributary drainage basin of the Yellow River, located in western Henan Province, China. Our 2011 fieldwork south of the Erlitou site in the Luoyang Basin indicates that an unconformity dating to ca. AD 1100 is roughly coincident with a major southward shift in the lower course of the Yellow River. In AD 1128, the governor of Kaifeng breached the dikes of the Yellow River to impede an advancing army, causing the Yellow River to flow south out to the Yellow Sea. We argue that the dike breach not only changed the fluvial dynamics of the Yellow River but also switched the rivers in the Luoyang Basin from an aggrading to an incising system. The resumption of sedimentation in the Luoyang Basin is roughly coincident with the next major shift of the Yellow River’s main course northward to the Bohai Sea in AD 1855. The unconformity found in the Luoyang Basin may be a legacy of historically contingent human agency rather than climatic shifts or gradual environmental modification.

Gao, Zongyu. "Zhengzhou Yellow River road-cum-railway bridge, China". Stahlbau 81, n.º 2 (febrero de 2012): 151–55. http://dx.doi.org/10.1002/stab.201201522.

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Xue, Chunting. "Historical changes in the Yellow River delta, China". Marine Geology 113, n.º 3-4 (agosto de 1993): 321–30. http://dx.doi.org/10.1016/0025-3227(93)90025-q.

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Dikötter, Frank. "Racial Identities in China: Context and Meaning". China Quarterly 138 (junio de 1994): 404–12. http://dx.doi.org/10.1017/s0305741000035815.

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This yellow river, it so happens, bred a nation identified by its yellow skin pigment. Moreover, this nation also refers to its earliest ancestor as the Yellow Emperor. Today, on the face of the earth, of every five human beings there is one that is a descendant of the Yellow Emperor.

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Tesis sobre el tema "Yellow River (China)":

Shi, Changxing y 師長興. "Sediment flux through the Yellow River sediment routing system". Thesis, The University of Hong Kong (Pokfulam, Hong Kong), 2002. http://hub.hku.hk/bib/B29851944.

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Lander, Brian. "Writing the environmental history of the Yellow River region from the Zhou to the Han : sources and methodological problems". Thesis, McGill University, 2006. http://digitool.Library.McGill.CA:80/R/?func=dbin-jump-full&object_id=99378.

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This thesis explores the changing environment of the middle and lower Yellow River basin from the Zhou to the reign of Han Emperor Wu (ca. 1045-87 B.C.), a period characterised by an increase of government control over the land along with an intensification and expansion of agriculture. The second chapter employs palaeoecological sources to look at the early environment of the region, arguing that the eastern plains were mixed forest-steppe, and that the regions to the west were mostly steppe. The third chapter uses archaeological sources to explore the rise of civilisation, the fauna of the region in the Shang period and the spread of iron tools. The fourth chapter is divided into two sections, the first of which looks at what can be learned from the texts of the period concerning agriculture, land clearance, deforestation, hunting, fishing and economic geography. The second half concerns the intensification of state power in regulating and transforming natural environments through legal measures and water control projects, as well as the development of a market economy.

Lingen, Carl y Nathan Buras. "Dynamic Management of a Surface and Groundwater System on Both Sides of the Lower Yellow River". Department of Hydrology and Water Resources, University of Arizona (Tucson, AZ), 1987. http://hdl.handle.net/10150/614178.

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This paper analyzes the management problem of the conjunctive use of surface and ground water in an irrigation system on both sides of the Lower Yellow River. For this purpose, a stochastic dynamic programming model is developed. In the model, the statistical characteristics of seasonal rainfall within 2 years are considered; groundwater level control is also emphasized in order to prevent soil salinity and waterlogging. Through computer calculations, optimal operation policies are obtained for efficient conjunctive use of surface and groundwater. These policies take into account the interactions between pumping groundwater by farmers, canal diversions by irrigation system managers, and the physical response of the stream- aquifer system, and minimize the total operation costs. In this paper, we take an irrigation district, the People's Victory Canal System, as an example to illustrate the development and solution of the model. At the same time, the effects of system parameters, including surface irrigation efficiency and rainfall recharge coefficient, on the optimal policies or total operation costs, are discussed. The analytical results in this example indicate that the variation in optimal operation costs caused by the proportion of rainfall infiltrated is small, but the effect of surface irrigation efficiency on the costs is significant. Hence, the surface irrigation efficiency must be increased as much as possible. Then, efficient conjunctive use of surface and groundwater can be attained with the optimal policies.

Liu, Peng. "InSAR observations and modeling of Earth surface displacements in the Yellow River Delta (China)". Thesis, University of Glasgow, 2012. http://theses.gla.ac.uk/3787/.

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Subsidence in river deltas is a complex process that has both natural and human causes (Boesch et al., 1994). The Yellow River delta is used for farming, contains an important nature reserve for wild animals especially for waterfowl, has a population of 1.64 million, and is the location of significant oil fields (Chen et al., 2012). Increasing human activities like farming and petroleum extraction are affecting the Yellow River delta, and one consequence is subsidence. This subsidence may have social, economic and environmental impacts (Syvitski et al., 2009). The purpose of this thesis is to measure the surface displacement in Yellow River delta and to investigate the causes of measured displacement. The use of Interferometric Synthetic Aperture Radar (InSAR) for Earth surface displacement mapping has increased since the 1990s when a lot of radar images become available. InSAR time series techniques identify displacement of an area between different image acquisition times. In this study, StaMPS package was employed to process Envisat ASAR images collected between 2007 and 2010. StaMPS selects only the stable pixels from interferograms to maintain the coherence signals over a long time interval. Consistent results between two descending tracks show subsidence with a mean velocity of up to 30 mm/yr in the radar line of sight direction in Gudao Town (oilfield), Gudong oilfield and Xianhe Town of the delta, and also show that subsidence is not uniform across the delta. Field investigation shows an association between areas of subsidence and of petroleum extraction. In a 9 km2 area of the Gu-Dao Oilfield in the delta, InSAR derived surface deformation is used to model the geometry, volume or pressure change of the deformation source, namely the extraction of fluids, using three different models: the spherical source Mogi type model, the finite prolate spheroid model and the poroelastic disk reservoir model. In general, good fits between InSAR observations and modelled displacements are seen. The source depths estimated in the three models agree well with the published oilfield depth. The subsidence observed in the vicinity of the oilfield is thus suggested to be caused by fluid extraction. For Mogi type model, a uniform subsidence rate of about 7 mm/yr is co-estimated. InSAR observations in Xianhe Town in the delta, which is not affected by oil extraction, also shows 8~12 mm/yr uniform subsidence. It is suggested this uniform subsidence is caused by other sources e.g. loading and sediment compaction. Since InSAR only measures relative displacement, accurate determination of small uniform rate need the reference phase provided by other observations e.g. GPS and levelling. Mogi model provides the volume change in Gudao oilfield. The ellipsoidal source and the disk reservoir model the pressure changes. Additional reservoir information e.g. material parameter will help better confine the model parameters. Although no production data is available for comparison, the volume and pressure changes obtained from the models, together with InSAR observed displacement might be of interest for oil industry, to predict future subsidence in Gudao oilfield.

Huybrechts, Nicolas. "Fully coupled 1D model of mobile-bed alluvial hydraulics: application to silt transport in the Lower Yellow River". Doctoral thesis, Universite Libre de Bruxelles, 2008. http://hdl.handle.net/2013/ULB-DIPOT:oai:dipot.ulb.ac.be:2013/210484.

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The overall objective is to improve the one-dimensional numerical prediction of the fine and non-cohesive bed material load in alluvial rivers, especially during high intensity episodes during which sediment beds are strongly remobilized. For this reason, we attempt to reduce the major inaccuracy sources coming from the alluvial resistance and bed material load relations needed to close the mathematical system. Through a shared parameter called the control factor m, the interactions occurring in alluvial rivers are incorporated more deeply into the mathematical model and more particularly into the closure laws: bed material load (SVRD, Suction-Vortex Resuspension Dynamics) and the energy slope (Verbanck et al. 2007). The control factor m is assumedly related to the Rossiter resonance modes of the separated flow downstream the bed form crest.

To further improve the representation of the flow-sediment-morphology interactions, a fully coupled model approach has been naturally chosen. In this work the terminology fully coupled means that the three equations forming the system are solved synchronously and that the terms often neglected by more traditional decoupled models are kept.

The feasibility of the new closure methodology has been drawn up by reproducing numerically the silt-flushing experiment conducted by the Yellow River Conservancy Commission (Y.R.C.C.) in the Lower Yellow River (LYR) in Northern China. The objective of the silt flushing experiment is to reverse the aggradation trend of the Lower Yellow River which, in the last decades, has become a perched river. The numerical simulation specifically reproduces the silt-flush effects in a reach of LYR located in the meandering part of the river. This reach (around 100 km) is delimited by Aishan and Luokou hydrometric stations.

Since the SVRD formulation has been developed from flume observations, the law has first been confronted to river datasets. The confrontation has revealed that the SVRD law becomes less suitable for fine sediment fluxes (ratio of water depth over median particle size > 5000). Therefore, a modified equation SVRD-2 has been built to enlarge the validity range.

The suitability of the SVRD-2 equation to predict fine sediment fluxes has been tested on data available from several hydrometric stations located in the meandering reach of the LYR: historical observations and measures collected during the flushes. The SVRD-2 has also been compared with relations specifically calibrated for this configuration. The comparison has pointed out that the performance of the two formulas is similar, which is encouraging for the SVRD-2 approach as it has not been calibrated on those data.

The closed equation system has been written on its quasi-linear form and is solved by a Finite Volume Method combined with a linearized Riemann algorithm. The numerical model has been checked up on two test cases: deposition upstream of a dam and the aggradation experiment conducted by Soni 1975.

As it is not yet possible to predict dynamically the value of the control factor m, a possible solution would be to extract its value from the measured data at the inlet cross section. Unfortunately, the necessary data are not measured locally. Moreover, a uniform value of the control factor m may not suffice to reproduce the flow along the whole reach. Therefore, it has been proposed to work temporarily in the reverse way.

From the comparison between the numerical results and the experimental data, a time evolution of the control factor m has effectively been extracted and it has been shown that it varies along the reach. At Aishan, the evolution of the control factor m corresponds to the evolution expected from the data analysis previously conducted on other data sets: the value of the control factor m decreases during the flush as it tries to reach the optimal value m=1. The time evolution at Luokou behaves differently to the one at Aishan, but remains in agreement with m evolution patterns observed historically for the river section flowing round Jinan City walls. For Luokou, the highlighted differences may come from three dimensional effects coming from the meander bend upstream the station.

Generally, the results obtained for the hydraulics, the sediment transport and bed adaptation are encouraging but still need improvements and additional feeding from the experimental data. The results for the concentration and therefore the bed elevation are very sensitive to the value of the control factor m as it influences most of the terms of the bed material load equation (SVRD-2).

The major remaining difficulties are, firstly, to deal with the rapid transients for which the model is less suitable and, secondly, to improve the prediction of the value of control factor m. Before paying more attention into the transients, enhancements concerning the flow along the reach (initial condition and discharge rates during the first days of the flush) must be conducted in priority. Indeed as the prediction of the bed or the cross section evolutions depend directly on the quality of the prediction of the sediment concentration and the hydraulics, one should first improve these aspects. To perform this study, more information about the water levels or sediment concentrations is necessary at some intermediate stations. One solution is to lengthen the studied reach, upstream to Sunkou and downstream to Lijin, totaling a river length of 456 Km.

A more entire signal of the energy slopes and the associated bed configurations at different stations would enlighten how the control factor m evolves along the reach during the silt-flush events.

Doctorat en Sciences de l'ingénieur
info:eu-repo/semantics/nonPublished

Leong, Elaine. "Water Situation In China - Crisis Or Business As Usual?" Thesis, Linköpings universitet, Industriell miljöteknik, 2013. http://urn.kb.se/resolve?urn=urn:nbn:se:liu:diva-94186.

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Several studies indicates China is experiencing a water crisis, were several regions are suffering of severe water scarcity and rivers are heavily polluted. On the other hand, water is used inefficiently and wastefully: water use efficiency in the agriculture sector is only 40% and within industry, only 40% of the industrial wastewater is recycled. However, based on statistical data, China’s total water resources is ranked sixth in the world, based on its water resources and yet, Yellow River and Hai River dries up in its estuary every year. In some regions, the water situation is exacerbated by the fact that rivers’ water is heavily polluted with a large amount of untreated wastewater, discharged into the rivers and deteriorating the water quality. Several regions’ groundwater is overexploited due to human activities demand, which is not met by local. Some provinces have over withdrawn groundwater, which has caused ground subsidence and increased soil salinity. So what is the situation in China? Is there a water crisis, and if so, what are the causes?This report is a review of several global water scarcity assessment methods and summarizes the findings of the results of China’s water resources to get a better understanding about the water situation. All of the methods indicated that water scarcity is mainly concentrated to north China due to rapid growth, overexploitation from rivers and reduced precipitation. Whereas, South China is indicated as abundant in water resources, however, parts of the region are experiencing water scarcity due to massive dam constructions for water storage and power production. Too many dam constructions in a river disrupts flow of the river water and pollutants are then accumulated within floodgates.Many Chinese officials and scholars believe that with economic growth comes improved environmental quality when the economy has reached to a certain of per-capita level. However, with the present water situation it is not sustainable or possible for China to keep consuming and polluting its water resources. Improvement of environmental quality does not come automatically with increased income, and policies, laws and regulations are needed in order to stop further deterioration of the environment.China’s water situation is not any news and the key factor is human activities, but the question is how to solve it. China’s water crisis is much more complex than over exploitation of groundwater and surface water. There are three water issues in China: “too much water – floods, too little water – droughts, and too dirty water – water pollution” (Jun & Chen, 2001). Thus, solving China’s water crisis is a huge challenge to solve without negatively affecting the economic growth.

Tan, Jiaxin [Verfasser]. "Industrial Water Pollution in Dongying City, the Yellow River Delta of China : Communication Interfaces between Government Agencies and the Local Population / Jiaxin Tan". Bonn : Universitäts- und Landesbibliothek Bonn, 2020. http://d-nb.info/1218301732/34.

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Gibbs, Levi Samuel. "Beyond the Western Pass: Emotions and Songs of Separation in Northern China". The Ohio State University, 2009. http://rave.ohiolink.edu/etdc/view?acc_num=osu1248745393.

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Hsieh, Tzung-Han y 謝宗翰. "Strategic Analysis and Planning over Television Industry in China: China Yellow River Television Case Study". Thesis, 2008. http://ndltd.ncl.edu.tw/handle/06526281500274423640.

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碩士
國立臺灣大學
企業管理碩士專班
96
A business operation varies in different domestic domain. To the nearby market- China, regarding to the similar culture and language, the fundaments of business is significantly different in Taiwan. As the economic boosts of mainland China, everyone is eagerly to get into China market, especially the media-industry, which is praised to be the “Next Cash Cow” of China. However, How to deal with the fundamental difference of business operation? It is a topic worthy to deeply study. The purpose of this thesis is focus in the Television Industry in China, proposing a complete strategic analysis with a real company- “China Yellow River Television” (CYRTV) to be a subject of case study and its future strategic development guideline. Here, the thesis begins with defining the business model of China TV industry, and conducting the macro-environment analysis. Then, by adopting “Porter’s Five Forces Model”, the thesis points out the industrial favorability. Based on the macro- and industrial- scope, identify the case company- CYRTV’s strengths and weaknesses through “Resource-based view”. Finally, combining internal and external forces with SWOT analysis, this thesis proposes strategies for the case company and its future roadmap. By analyzing the business model of TV industry in China, the thesis proposes the specification of the industry, and expressing the macro-environment status. Facing relatively strong regulation of government, the TV station in China has different industrial status-quo due to its level-of-operating. As to the case company- CYRTV, it is a central-level TV station that induces a much better resource status than most of other competitors. However, the existing channel penetration is low. How does CYRTV take its best advantage from resource-strength to cover resource-weakness, while extracting more profit in industrial-opportunity and avoid the threat of industry-force? This thesis states several strategic guidelines for CYRTV by using SWOT-matrix analysis. As a result, this thesis concludes that, CRYTV should leverage its status of central-level TV station and the unique positioning of official-out-country TV station, to penetrating the market while building quality of content, establishing the mind-relatedness to viewers. Meanwhile, leverage the close relationship with government, to approve the new-media’s license, constructing a platform business. This thesis conducts a complete strategic analysis over TV industry in China, with a real company – CYRTV as a case-study, discovering the status of TV industry in China, expecting to initiate industrial research of the media industry in China while providing a true reference for who interested to operating business in China.

McCain, Cynthia N. "Soil changes after afforestation in Yellow River loess : a case study in Gansu Province, People's Republic of China /". 1987. http://hdl.handle.net/1957/11020.

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Libros sobre el tema "Yellow River (China)":

Dodgen, Randall A. Controlling the dragon: Confucian engineers and the Yellow River in the late imperial China. Honolulu: University of Hawai'i Press, 2001.

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Pan, Xiandi. Sanmenxia shui ku xiu jian hou huang he xia you he chuang yan bian. 8^a ed. Zhengzhou Shi: Huanghe shui li chu ban she, 2006.

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Chen, Jitao. Huang He he kou shui wen ce yan. 8^a ed. Zhengzhou Shi: Huang He shui li chu ban she, 2008.

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Jinqing, Cao. China along the Yellow River: Reflections on rural society. New York: RoutledgeCurzon, 2004.

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Sinclair, Kevin. The Yellow River: A 5000 year journey through China. London: Weidenfeld and Nicolson, 1987.

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Sinclair, Kevin. The Yellow River: A 5000 year journey through China. Los Angeles, Calif: Knapp Press, 1987.

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Zhang, Chunli. Yu Huang He yi qi zou guo. 8^a ed. Zhengzhou Shi: Huang He shui li chu ban she, 2009.

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Zhang, Ange. Red land, Yellow River: A story from the Cultural Revolution. Toronto: Groundwood Books, 2004.

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Wang, Kaichen. Huang He he kou de yan bian yu zhi li. 8^a ed. Zhengzhou Shi: Huang He shui li chu ban she, 2010.

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Hu, Chunhong. Huang He shui sha tiao kong yu xia you he dao zhong shui he cao su zao. 8^a ed. Beijing: Ke xue chu ban she, 2007.

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Capítulos de libros sobre el tema "Yellow River (China)":

Lijuan, Cui, Zhang Manyin y Xu Weigang. "Huang He (Yellow River) River Basin (China)". En The Wetland Book, 1–14. Dordrecht: Springer Netherlands, 2016. http://dx.doi.org/10.1007/978-94-007-6173-5_98-1.

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Lijuan, Cui, Zhang Manyin y Xu Weigang. "Huang He (Yellow River) River Basin (China)". En The Wetland Book, 1575–88. Dordrecht: Springer Netherlands, 2018. http://dx.doi.org/10.1007/978-94-007-4001-3_98.

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Ma, Xieyao, Yoshinobu Sato, Takao Yoshikane, Masayuki Hara, Fujio Kimura y Yoshihiro Fukushima. "Hydrological Analysis of the Yellow River Basin, China". En Climatic Change and Global Warming of Inland Waters, 67–78. Chichester, UK: John Wiley & Sons, Ltd, 2012. http://dx.doi.org/10.1002/9781118470596.ch4.

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Shen, Dajun. "Water Resource Allocation and Regulation in Yellow River Basin". En Water Resources Management of the People’s Republic of China, 291–306. Cham: Springer International Publishing, 2020. http://dx.doi.org/10.1007/978-3-030-61931-2_14.

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Zhou, Kuiyi y Jun Deng. "Pan Jixun and the Ancient Governance Plan of the Yellow River". En The Studies of Heaven and Earth in Ancient China, 203–50. Singapore: Springer Singapore, 2021. http://dx.doi.org/10.1007/978-981-15-7841-0_6.

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Cui, Baoshan, Qichun Yang, Kejiang Zhang, Xinsheng Zhao y Zheyuan You. "Responses of saltcedar (Tamarix chinensis) to water table depth and soil salinity in the Yellow River Delta, China". En Plant Ecology in China, 99–110. Dordrecht: Springer Netherlands, 2010. http://dx.doi.org/10.1007/978-90-481-9993-8_9.

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Zhang, Jianfeng. "Responses of Plant Community Change on Wetland Degradation in Yellow River Delta Region". En Coastal Saline Soil Rehabilitation and Utilization Based on Forestry Approaches in China, 165–79. Berlin, Heidelberg: Springer Berlin Heidelberg, 2013. http://dx.doi.org/10.1007/978-3-642-39915-2_18.

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Zhang, Jianfeng. "Strategies for Reclaiming and Ameliorating Saline Soil in the Yellow River Delta Region". En Coastal Saline Soil Rehabilitation and Utilization Based on Forestry Approaches in China, 55–64. Berlin, Heidelberg: Springer Berlin Heidelberg, 2013. http://dx.doi.org/10.1007/978-3-642-39915-2_7.

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Liu, Xiaolei, Yonggang Jia, Jiewen Zheng, Lei Guo y Hongxian Shan. "Dynamic Processes of the Benthic Boundary Layer in the Subaqueous Yellow River Delta, China". En Engineering Geology for Society and Territory – Volume 4, 109–14. Cham: Springer International Publishing, 2014. http://dx.doi.org/10.1007/978-3-319-08660-6_21.

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Xu, Xuegong, Xiaofeng Duan, Richard Dawson, Yanhua Liu, Yu He, Huifang Peng y Chaowei Cui. "Effects of Lucc Resulting From Tffp Land Usepattern in the Yellow River Delta, China". En IFIP Advances in Information and Communication Technology, 431–41. Boston, MA: Springer US, 2009. http://dx.doi.org/10.1007/978-1-4419-0209-2_45.

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Actas de conferencias sobre el tema "Yellow River (China)":

Han, Mei, Yi Wang y Renqing Wang. "Health diagnosis for the Yellow River delta wetland, China". En 2011 Second International Conference on Mechanic Automation and Control Engineering (MACE). IEEE, 2011. http://dx.doi.org/10.1109/mace.2011.5987417.

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Yu, Shaw L., Jenny X. Zhen, Jen-Tai Yang, Richard Field y Dan Sullivan. "Planning for Wetland Protection and Restoration in the Yellow River Delta in China". En Wetlands Engineering and River Restoration Conference 2001. Reston, VA: American Society of Civil Engineers, 2001. http://dx.doi.org/10.1061/40581(2001)50.

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Wang, S., Y. Huang y G. Wang. "Study on Eco-environmental Synthetic Evaluation in Yellow River Basin, China". En 2006 IEEE International Symposium on Geoscience and Remote Sensing. IEEE, 2006. http://dx.doi.org/10.1109/igarss.2006.874.

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Zhu, Tingju, Ximing Cai y Claudia Ringler. "Dry Season Water Management in the Lower Yellow River in China". En World Environmental and Water Resources Congress 2011. Reston, VA: American Society of Civil Engineers, 2011. http://dx.doi.org/10.1061/41173(414)313.

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Xianglian Li, Xiusheng Yang, and Yuzhou Luo, Suocheng Dong, Chuansheng Wang y Xinan Deng. "Farming Productivity and Resources Sustainability in the Yellow River Basin, China". En 2003, Las Vegas, NV July 27-30, 2003. St. Joseph, MI: American Society of Agricultural and Biological Engineers, 2003. http://dx.doi.org/10.13031/2013.13839.

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Hu, Yong, Liangyun Liu, Lingling Liu, Quanjun Jiao y Jianhua Jia. "Mapping land cover of the Yellow River source using multi-temporal Landsat images". En Seventeenth China Symposium on Remote Sensing. SPIE, 2010. http://dx.doi.org/10.1117/12.910403.

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Zhi Yang, Yangxiao Zhou, Jochen Wenninger y Stefan Uhlenbrook. "Analysis of stream flow characteristics of the Hailiutu River in the central Yellow River, China". En 2011 International Symposium on Water Resource and Environmental Protection (ISWREP). IEEE, 2011. http://dx.doi.org/10.1109/iswrep.2011.5893124.

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He, Li. "Fluvial Characteristics of Sediment-Laden Flow in the Lower Yellow River, China". En World Environmental and Water Resources Congress 2016. Reston, VA: American Society of Civil Engineers, 2016. http://dx.doi.org/10.1061/9780784479872.032.

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Yunchao Jiang y Zhongren Nan. "Assessment of river water quality using uncertainly mathematical model: A case Study of Yellow River, China". En 2012 International Symposium on Geomatics for Integrated Water Resources Management (GIWRM). IEEE, 2012. http://dx.doi.org/10.1109/giwrm.2012.6349563.

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Chang, Fangqiang, Yonggang Jia, Hongxian Shan y Tao Liu. "The Study on Property Non-Uniformity of Superficial Sediment at the Yellow River Estuary, China". En ASME 2009 28th International Conference on Ocean, Offshore and Arctic Engineering. ASMEDC, 2009. http://dx.doi.org/10.1115/omae2009-79212.

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Resumen

The silt carried by the Yellow River accumulates rapidly at the estuary to form an underwater delta, and the sediment is influenced and transformed continuously by river and ocean dynamic forces. One-meter-deep superficial sediment samples were taken at the Yellow River estuary to measure the basic physical and mechanical properties in the laboratory. The laboratory tests revealed the superficial sediment is over-consolidated and the over-consolidation ratio (OCR) reduces with depth. Soil penetration resistance was measured by a Proctor Penetrometer In-Situ. The results show the strength of superficial sediment appear to be strong non-uniformity (variation), and the strength of Xin Tan and Guang Li Gang region is less than those of the Da Wang Bei and Diao Kou. Then, the extent of soil property non-uniformity in space was calculated according to the Vanmarcke Foundation Random Theory. The vertical non-uniformity size lies between 0.32–0.93m, with little difference between those of terrestrial soils, and the horizontal lies between 12–32m, less than those on land. Finally, the reasons to cause strong non-uniformity are discussed. They are mainly composed of sediment modification by wave and biological activities.