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1.
The erosion mechanisms of abandoned coastal section are understood detailedly by flume experiment, which play an important
role to the offshore engineering facilities. A movable-bed physical model has been used to investigate the coastal erosion
of an abandoned section of the Huanghe (Yellow) River Delta. The theory of physical scale models is discussed and a method
for constructing the representative seabed section is developed. The results indicate that during the period initially after
the abandonment of the delta the entire bed experienced rapid erosion because the seabed was steep and prone to liquefaction
that resulted from storm wave action. After this initial period, a balance of erosion and accretion was established, and the
beach profile equilibrated with a point of balance present on the profile. The experimental results indicate that the volume
of deposition was about half that of the erosion. Wave action may also induce significant stratal changes through its interaction
with the soft seabed. The major morphological features developed in the model delta section were found to be qualitatively
comparable with those observed in the prototype. A distorted modeling law that maintains the similarity of the modeled and
prototype equilibrium beach profiles is proposed. Experimental results show that the distorted modeling is able to reproduce
the beach-face slope in nature, and the model also successfully reproduced three historical evolutionary stages of erosion. 相似文献
2.
3.
Vuong Van Bui Daidu Fan Dac Ve Nguyen Dinh Lan Tran Duc Thanh Tran Van Long Hoang Thi Hong Hanh Nguyen 《中国海洋大学学报(英文版)》2018,17(6):1272-1280
Coastal erosion has become a worldwide concern, typically in the densely populated Asian mega-river deltas. Severe coastal erosion in the southern Red River Delta(RRD) has been intensively studied. Coastal morphological change in the northern RRD was examined in detail through DEM(Digital Elevation Model) analysis based on time series of bathymetrical maps(1965–2004) and Landsat images(1975–2015) in this study. The results show that the northern RRD is featured by rapid coastal accretion in the past few decades, although suspended sediment flux has dropped by roughly 60% after the completeness of Hoa Binh Dam(HBD) in 1988 and relative sea level rose at 1.9 mm yr~(-1). However, accretion at the outer part of subtidal shoals and platforms was observed to slow down quickly or even turned into erosion in the last two decades. The resuspended sediments from the erosion zone can be transported landward to replenish the inner coastal zone, keeping the latter accretion in the near future to compensate for the sediment discharge decrease from the river. However, this lag effect should be terminated soon if other adverse effects go worse, e.g., damming rivers, sea-level rising, strengthening storms, land reclamation and other poor-designed coastal engineering. Coastal planners and managers should pay full attention to these changes. 相似文献
4.
《中国地理科学(英文版)》2019,(2)
Coastal regions are threatened by natural processes, such as erosion driven by storm surges and the effect of jetties, as well as by human behavior. The coastline of the Yellow River Delta(YRD) was monitored using the general high-tide line method, which combines Remote sensing(RS) and geographic information system(GIS) technology, using multi-spectral scanner(MSS), thematic mapper(TM), and enhanced thematic mapper plus(ETM+) images of the YRD from 1976 to 2014 as a data source. The results demonstrated that the shape and length of the YRD coastline has changed dramatically since 1976. The course of the Diaokouhe channel has resulted in mainly inland erosion in the north, and is primarily marine erosion; therefore, it was termed an erosion-type estuary. However, the coastline of the Qingshuigou course has moved seaward, demonstrating an accretion stage, and was therefore termed an accretion-type estuary. The coastline advanced forward before 1997 and shrank after 2003 in the southern part of the river mouth, which was due to the shift in the river mouth in 1996. It has continually extended outward in the northern part of the river mouth from 2003 onward. The coastline in the southern part of the river mouth has moved randomly, with the occurrence of both erosion and sedimentation caused by land reclamation and sea wave intrusion. In most cases, the coastline has extended offshore, especially in the northern part of the river mouth. The YRD coastline has changed frequently and rapidly from 1992 to 2014. The river mouth channel, river water and sediments, and precipitation were the major factors affecting the YRD. The YRD coastline was mainly in an accretion stage during flow periods. The erosion rate decreased and tended to be stable during a dry period. The coastline was basically stable when dry periods occurred over a long period. The location of Yellow River ports and sea erosion were the main factors driving coastline changes. The coastline was mainly influenced by the flow path of the Yellow River, with recent human activity also becoming a factor. 相似文献
5.
XUEChunting 《中国海洋大学学报(英文版)》2005,4(2):115-123
Studies on land loss in Tuvalu reveal the following findings. Although both sea level rise and coastal erosion can cause land loss in the tropic Pacific oceanic islands, their mechanisms are different. When sea level rises, the low elevation coastal zone submerges and the erosion datum plane rises, the beach process progresses normally as always, resulting in no beach sediment coarsening. When the sea level is stable, coastal erosion removes finer sediment from reef flat, beach and land, resulting in beach sediment coarsening. The human-induced coastal erosion in the tropic Pacific oceanic islands has the following features. 1) Erosion occurs or intensifies immediately after inappropriate human activities. 2) It occurs near the places having human activities and places related to the above places in sediment supply. 3) It often occurs on original prograding or stable coasts (on lagoon coasts for atolls) because there are more coastal engineering projects and other human activities on such coasts. 4) It is chronic, covering a long period of time. The coastal geological events in Tuvalu islands do not accord with the features resulted from sea level rise but do accord with the features resulted from coastal erosion, particularly from human-induced erosion. The land loss in Tuvalu is mainly caused by inappropriate human activities including coastal engineering and aggregate mining, and partly caused by cyclones. Moreover, all recent measurements (satellite altimetry,thermosteric sea level data and tide observations) so far have not been able to verify any sea level rise around Tuvalu islands. 相似文献
6.
Roads are conspicuous components in a river landscape;however,their impacts on river landscape patterns and ecological processes have not been systematically studied at the watershed scale.In this paper,the Lancang River Valley in Yunnan Province,China was selected as a case to study road lateral disconnection and crossing impacts and identify river-road network interaction.This study was primarily focused on the road impacts on soil erosion intensity and patch density by using GIS analysis at different scales and explored their distribution with terrain factors.The results showed that river density revealed spatial autocorrelation although both of the roads and rivers were distributed unevenly in the valley.The lateral road(road curvature≥1.1)proportion correlated with soil erosion intensity(p 0.01)at the small sub-basin scale.Soil erosion intensity decreased with increasing lateral road buffer width.Light erosion generally accounted for a large proportion of the erosion in the lateral road buffer zones(1.0–4.0 km),while higher class lateral roads imposed greater impacts on soil erosion than lower class roads,which primarily had a moderate erosion level.In addition,the results of road-river intersection density indicated that road crossing impacts were significantly correlated with patch density at the small sub-basin scale.Topography factor(percent of slope25°in each sub-basin had a close relationship with the ratio of total length of road line with curvature value≥1.1 to the total number of intersections.The correlation(p 0.01)between road impacts and terrain factor revealed that topography affected the road impact distribution in the Lancang River Valley. 相似文献
7.
The morphology of the beach backshore and foreshore at Huiquan Bay, Qingdao, China, is characterized by a single intertidal
sandbar system with a spring tide range of 4.59 m. The beach was measured with a laser total station of Leica TPS402. Contours
of the beach were generated using data collected in March and November 2005. The survey method provided 2 mm measuring accuracy
and 4–10 m horizontal spacing. The net accretion volume of the foreshore was about 11, 215 m3 from March to November. After sand sculpture activity, the axis of the sand trough migrated onshore from about 3.5 m to 17.5
m on the foreshore beach in November. At the same time, the axis of the sandbar crest migrated onshore no more than 42.25
m on the northwest foreshore; and it migrated offshore no more than 23.75 m on the southeast foreshore. On the northwest and
southeast foreshore beach, two strips of erosion areas with a thickness of 0–0.2 m appeared on the sandbar crest. Accretion
occurred at the bottom of the sand trough with a thickness of ∼0.2–0.6 m. The sandbar height decreased after sand sculpture
activity, and it was no more than 0.7 m in March and 0.6 m in November. Human activities, such as sand digging on the sandbar
crest during sand sculpture activity, also can disturb the beach morphology of intertidal bar systems. This phenomenon also
was validated by comparison of beach morphology, the results of a color artificial tracer experiment and a sediment transportation
trend prediction. 相似文献
8.
In China,gravity retaining walls are widely used as protection structures against rockfalls,debris flows and debris avalanches along the roads in mountainous areas.In this paper,the Discrete Element Method(DEM) has been used to investigate the impact of granular avalanches and debris flows on retaining walls.The debris is modeled as two dimensional circular disks that interact through frictional sliding contacts.The basic equations that control the deformation and motion of the particles are introduced.A series of numerical experiments were conducted on an idealized debris slide impacting a retaining wall.The parametric study has been performed to examine the influences of slope geometry,travel distance of the sliding mass,wall position,and surface friction on the impact force exerted on the wall.Results show that:1) the force achieves its maximum value when slope angle is equal to 60°,as it varies from 30° to 75°;2) an approximate linear relationship between the impact force and the storage area length is determined. 相似文献
9.
Ji Zixiu 《中国地理科学(英文版)》1994,(4)
（季子修）（蒋自巽）ＩＭＰＡＣＴＳＯＦＳＥＡＬＥＶＥＬＲＩＳＥＯＮＣＯＡＳＴＡＬＥＲＯＳＩＯＮＩＮＴＨＥＣＨＡＮＧＪＩＡＮＧＲＩＶＥＲＤＥＬＴＡＡＮＤＮＯＲＴＨＪＩＡＮＧＳＵＣＯＡＳＴＡＬＰＬＡＩＮＯ￥ＪｉＺｉｘｉｕ（ＮａｎｊｉｎｇＩｎｓｔｉｔｕｔｅ... 相似文献
10.
At present, approximately 36% of coasts are experiencing net erosion in the Changjiang River delta and the north Jiangsu coastal
plain. Future sea level rise will accelerate the process of coastal erosion. According to the ratio of the calculated value
of coast retreat by Bruun rule to the estimated value by using measured data, the proportion affected by sea level rise in
total coastal erosion has been estimated in this paper. When sea level rises by 20cm, the proportion determined by sea level
rise will increase from 1.0% at present to 2.2% in the future in the coasts of abandoned Huanghe River delta and from 8.5%–9.6%
to 13.5%–15.2% in the north and south banks of the Changjiang River delta. This result is lower than that from the similar
research in the world, and this phenomenon is related with the special development process of the coasts in this area. The
mechanism of accelerating coastal erosion by sea level rise is that sea level is will increase the intensity of tidal current,
wave and storm surge and decrease the ability to reduce the force of waves on the tidal flat and coastal wetland due to the
loss of their areas. Therefore, the length of erosion coasts will increase, the sedimentation rate of accretion coasts will
decrease or even turn accretion into erosion, the width of tidal flat will reduce and coastal slope will increase. So the
project of coastal protection of this area must be reinforced.
Project funded by the National Natural Science Foundation of China and the Chinese Academy of Sciences. 相似文献
11.
黄河三角洲是陆海交界地带,陆地海洋相互作用显著,泥沙所引起的岸滩演变、港口航道的淤积、水动力环境的改变等问题比较复杂。该文采用三维HEM-3D数值模型对黄河三角洲海域流场变化、盐度、悬浮泥沙浓度及海岸冲淤分布进行了潮流周期内的数值模拟分析。结果表明,黄河三角洲海域的悬浮泥沙浓度分布与潮流场变化和河口泥沙输入有密切的关系,在三角洲北部受五号桩外强潮流区的影响,近岸海底的泥沙发生明显的再悬浮,并在涨潮流向南输送,含沙量达1.5 g/L左右。在三角洲南部(现行河口区域和莱州湾区域),受现行河口入海泥沙扩散的影响显著。海域年冲淤分布,在北部废弃三角洲区域,由于海洋动力作用强烈,浅水冲刷,海底侵蚀显著,形成了明显呈沿岸展布的侵蚀中心,在侵蚀中心以外,侵蚀快速减弱。在现行河口区域,以淤积为主,在羽状流扩散的控制下,泥沙入海后向南输运,至莱州湾区域逐渐减弱。数值模拟的结果与卫星遥感解译的岸线变化基本一致,效果良好。 相似文献
12.
本文选择黄河三角洲大汶流自然保护区为研究对象,以多时相遥感影像,对土地利用类型进行解译分析。同时,以平均低潮线作为分析基线,提取海岸线变化信息。结果表明:1996-2009年研究区面积净增13.35km2。各种土地利用类型中滩涂所占面积最大,养殖池所占比例最小,但增幅明显。芦苇地面积后期增长迅速,指示研究区生态环境趋向转好。自然因素(黄河来水来沙量)和人类活动(黄河调水调沙工程,湿地恢复工程,滩涂规模开发以及人类开垦造田)是研究区土地利用类型变化的直接驱动力。1976-2009年研究区海岸净造陆面积217.14km2,沙嘴变幅为29.2km。黄河入海水沙量和滨海区的海洋潮流条件共同影响着海岸线的变迁。 相似文献
13.
Soil Erosion under Different Land Use Types and Zones of Jinsha River Basin in Yunnan Province, China 总被引：4，自引：1，他引：3
YANGZisheng LIANGLuohui 《山地科学学报》2004,1(1):46-56
Severe soil erosion in the middle and upper reaches of Yangtze River has been regarded as a major environmental problem. The on-site impact of soil erosion on agricultural production and the off-site impact on floods and sedimentation in Yangtze Rive are well known. A quantitative assessment of soil erosion intensity is still scanty for developing appropriate soil erosion control measures for different land use types and zohes in this region. This article constructs a localized USLE and estimates the average soil loss in the Jinsha River Region in Yunnan Province, one of the priority areas for soil erosion control in the middle and upper reaches of Yangtze River. The estimation is done under different land uses and zones in this basin. The estimation shows that while soil erosion in the cultivated land is the most severe, 36～40% of the garden and forest land suffers from soil erosion of various degrees due to lack of ground cover and other factors. Soil erosion in the pasture is modest when the ground cover is well maintained. It also confirmed that terracing can reduce soil erosion intensity significantly on the cultivated land. Research findings suggest that sufficient attention must be paid to regeneration of the ground cover in reforestation programs. In addition to mass reforestation efforts, restoration of grassland and terracing of the cultivated land should also play an important role in erosion control. 相似文献
14.
HU Guanghai ) * YAN Tong ) WANG Xiuqin ) ZHONG Delin )) First Institute of Oceanography S.O.A. Qingdao P..R.China) Ocean University of China Qingdao P..R.China 《中国海洋大学学报(英文版)》2004,3(2):195-200
1 Introduction Manhasmodifiedmanyoftheworld’scoastlines ,eitherdirectlybyconstructionordredging ,orindi rectlyasaresultofenvironmentalchangesthatinflu encesedimentsupply ,runoff,orclimate (Johns ,1995 ) .HumanactivityhasalsoproducedthemostprofoundeffectsonthecoastalenvironmentinChina .Forex ample,damconstructions ,whichrestrictpeakflowsintheupstreamoftheYellowRiver ,couldgreatlyre ducethenaturalsupplyofsedimentintotherivermouthandresultintheerosionofbeaches . Inrecentyears,manystudiescon… 相似文献
15.
Cuiping Kuang Yue Ma Binyu Wang Jueyi Sui Jie Gu Jianhui Liu Gang Lei 《中国海洋大学学报(英文版)》2018,17(6):1290-1300
Breakwaters can be used as artificial headlands in beach nourishment to mitigate coastal erosion. Longfengtou Beach, located on the southwest coast of Haitan Bay facing the Taiwan Strait on the northeast, suffers severe erosion, where the monsoon causes significant season hydrodynamic variations. Headland breakwaters are intended to be employed to mitigate coastal erosion. A 2D sediment transport model is established using MIKE21 based on current-wave coupling and calibrated by measured data. Summer and winter wave conditions are chosen as characteristic weak and strong waves respectively. The numerical results of suspended sediment concentration and seasonal morphological evolution are compared under the conditions with and without the headland breakwaters. Sediment transport in summer can be regarded as mainly determined by current field, while in winter wave effect is strong enough to change current field. The northern breakwater, nearly perpendicular to the ebb current direction, obstructs the currents and decreases velocity of the ebb currents, and confines the water carrying sediments within the protection area during the flood period. The southern breakwater also breaks the waves in advance and significantly reduces the hydrodynamic effects during the flood period and maintains high suspended sediment concentration in the protection area. In general, two headland breakwaters decrease the erosion near the beach and enlarge the deposition area, which play a significant role in prevention of sediment loss in nearshore area and mitigate coastal erosion. 相似文献
16.
Spatial structure and land use control in Extended Metropolitan Region of Zhujiang River Delta,China 总被引：1，自引：0，他引：1
The Zhujiang (Pearl) River Delta is one of the most developed Extended Metropolitan Regions (EMR) in China.With the rapid urbanization,the agglomeration of population and industries has emerged,which has led to dramatic changes of spatial structure and land use in this region.With data of high resolution TM remote sensing images and Google Earth maps,this paper identified and analyzed the spatial pattern of the Zhujiang River Delta EMR using Envy and ArcGIS tools.It was found that 1) the industrial land uses were expanding substantially,particularly on the bank sides of the Zhujiang River estuary;2) large-scale housing developments were concentrated in the fringe of metropolitan areas such as those of Guangzhou and Shenzhen;3) a regional transportation network with the spatial pattern of ″1 circle +2 pieces + 3 axes″ had significantly affected the location choice of manufacture enterprises.At the same time,both highly specialized land use and severely mixed land use patterns were identified.As a consequence of the latter,land use efficiency of the whole EMR areas was reduced.Moreover,ecologic and environmental problems were severe.Based on the above analysis,suggestions were given from the viewpoint of spatial safety,land use efficiency,and the reorganization of spatial structure in the Zhujiang River Delta EMR. 相似文献
17.
As part of a collaborative study between the 3rd Institute of Oceanography, Xiamen, and the U. K. Universities of East Anglia
and St. Andrews, a 4-day experiment was conducted on a ridge- and- runnel beach of north Norfolk on the North Sea coast. Detailed
surveys were made of every low water of an area 10m by 30m and electromagnetic current meters were used to measure wave-induced
currents over the ridge and in the runnel. The locations of bedform fields were noted, fluorescent sand was used to follow
the sand movement and, at the end of the experiment, lacquer peels were taken of the top 0.2m of a vertical section through
the ridge- and- runnel.
During the 4 days 0.75m3 of sand per metre width of beach accreted in the runnel and a similar volume was eroded from the upper foreshore. The dominant
shoreward transport, identified qualitatively by the movement of the fluorescent sand, suggests the ridge- and- runnel system
migrated shorewards up the general beach slope of 1o by 2–3m. The wave orbital currents were used to predict the bedforms to be expected over the tidal cycle: an upper phase
plane- bed was predicted for most of the period but vortex and rolling- grain ripples were predicted and observed when the
water level over the ridge was low. As the tide dropped ripples on the ridge were eliminated by swash action but the ripples
in the runnel were protected by the ridge and remained on the beach after the tide dropped.
The observed accretion of the beach in the runnel and on the lee slope of the ridge was used to calculate that a net average
shoreward transport of 0.11g/cm·s−1 occurred over the ridge crest during the period it was underwater. The current meter measurements of the wave orbital currents
and the mean currents over the ridge crest were used with the wave- current interaction model of Grant and Madsen (1982),
ripple dimensions defined by Nielsen (1981), and resuspension coefficient of Vincent and Green (1990), to compute bedload
sand transport rates from the equations of Madsen and Grant (1976), Sleath (1978), and Vincent et al. (1981), and also the
suspended sand transport rates. The results from one of these bedload equations (Madsen and Grant, 1976) compared well with
the observed net transport. The calculated suspended load transport rates (due to steady currents alone) were a factor of
5 too great, and were also several orders of magnitude greater than suspended transport rates measured directly under similar
or more energetic wave and current conditions. 相似文献
18.
为研究动态热条件下不同结构材料的建筑墙体热性能和保温厚度优化问题,针对大庆地区冬季气候特征,建立墙体非稳态传热模型,分析分别采用Concrete、Briquette、Brick、Blokbims、AAC等5种结构材料和挤塑聚苯乙烯EPS、泡沫聚苯乙烯XPS等2种保温材料的建筑墙体热性能,计算大庆地区1月典型日的室外综合温度并进行各种墙体传热分析和保温厚度优化.结果表明:冬季最大温度波动和峰值负载发生在Concrete结构材料墙体中,其次是Briquette、Brick、Blokbims和AAC结构材料墙体中,且在相同情况下AAC结构材料墙体的保温效果明显优于其他结构材料墙体;综合考虑影响保温层经济厚度的主要因素,通过经济分析计算,得出在相同经济条件下、大庆地区采用5种不同结构材料240mm厚度墙体保温时的最优保温厚度,为建筑墙体工程应用提供指导. 相似文献
19.
The headland-bay beach is one of the most common coastal types in the world.Its morphology reflects the changes that occurred during long-term evolution of the sandy coast.Several headland-bay beach models have been proposed to simulate the coastline’s configuration in equilibrium.In this paper,a new elliptical model is proposed,described,and applied.On the east coast of Laizhou Bay in Shandong Province from Longkou Port to Diaolongzui,four typical headland-bay beaches have developed,and four headland-bay beach models are used in this paper to simulate the morphology of these beaches to assess the applicability of each model.The simulation results of the elliptical model verify that it is applicable to the study area.In addition,the elliptical model is easy to use.Through simulation and field investigations,we concluded that most of the coastal segments in this area will remain in an erosion state,and the human activity has a significant impact on the shoreline’s evolution. 相似文献
20.
三北地区是我国重要的生态屏障,分析2000—2019年三北防护林体系建设工程（简称：三北工程）区植被恢复时空变化状况,厘定人类活动与气候要素对植被恢复的贡献,探究植被恢复对土壤风蚀影响,评估植被恢复潜力空间,可为三北防护林体系建设工程未来规划管理和科学施策提供参考。本文在选取植被覆盖度和植被净初级生产力表征植被恢复状况基础上,利用地面数据,结合模型模拟,定量评估了2000—2019年三北防护林体系建设工程区植被恢复程度及其对土壤风蚀的影响,并对植被恢复潜力进行探究。研究结果表明：① 2000—2019年植被恢复程度高、较高的面积,占总面积的35.29%和13.16%,主要分布在黄土高原区及北部区域和风沙区与东北华北平原农区的部分地区。人类活动与气候因素对植被恢复贡献率为10.45%和89.55%;② 土壤风蚀以轻度侵蚀和微度侵蚀为主,呈逐年下降趋势,剧烈侵蚀面积减少了66.45%,防风固沙服务得到进一步提升。植被恢复程度与土壤风蚀模数呈负相关关系,植被恢复程度较好有助于降低土壤风蚀模数;③ 三北工程区森林、草地和荒漠生态系统仍有8.16%的恢复潜力,内蒙古高原北部部分地区、哈顺戈壁北部和准噶尔盆地西北部及周边区域、黄土高原南部部分区域存在较大恢复潜力。 相似文献