人民长江
人民長江
인민장강
YANGTZE RIVER
2015年
15期
14-17
,共4页
乔红杰%杜国元%朱巧云%张志林
喬紅傑%杜國元%硃巧雲%張誌林
교홍걸%두국원%주교운%장지림
澄通河段%床沙%粒度%中值粒径%长江口
澄通河段%床沙%粒度%中值粒徑%長江口
징통하단%상사%립도%중치립경%장강구
Chengtong reach%bed material%particle size%median particle size%Yangtze River estuary
为了进一步研究长江口水土资源和岸线开发利用工作对该段河床演变和水动力变化的影响,根据2012年及2013年枯水期长江口澄通河段两次大范围床沙取样监测成果,分析了各主支汊床沙的物质组成,粒度分布及丰枯水年粒度特征。结果表明:澄通河段主槽砂粒粗,浅滩砂粒细;主汊砂粒粗,支汊砂粒细;总体上,从上游向下游床沙粒度逐渐变细;主槽及主汊区域床沙类型主要为细砂及粉砂质砂,支汊及浅滩区域床沙类型主要为砂质粉砂及黏土质粉砂;2012年,全河段床沙的粒度组成表现为,砂含量大于粉砂含量,粉砂含量大于黏土含量。
為瞭進一步研究長江口水土資源和岸線開髮利用工作對該段河床縯變和水動力變化的影響,根據2012年及2013年枯水期長江口澄通河段兩次大範圍床沙取樣鑑測成果,分析瞭各主支汊床沙的物質組成,粒度分佈及豐枯水年粒度特徵。結果錶明:澄通河段主槽砂粒粗,淺灘砂粒細;主汊砂粒粗,支汊砂粒細;總體上,從上遊嚮下遊床沙粒度逐漸變細;主槽及主汊區域床沙類型主要為細砂及粉砂質砂,支汊及淺灘區域床沙類型主要為砂質粉砂及黏土質粉砂;2012年,全河段床沙的粒度組成錶現為,砂含量大于粉砂含量,粉砂含量大于黏土含量。
위료진일보연구장강구수토자원화안선개발이용공작대해단하상연변화수동력변화적영향,근거2012년급2013년고수기장강구징통하단량차대범위상사취양감측성과,분석료각주지차상사적물질조성,립도분포급봉고수년립도특정。결과표명:징통하단주조사립조,천탄사립세;주차사립조,지차사립세;총체상,종상유향하유상사립도축점변세;주조급주차구역상사류형주요위세사급분사질사,지차급천탄구역상사류형주요위사질분사급점토질분사;2012년,전하단상사적립도조성표현위,사함량대우분사함량,분사함량대우점토함량。
To further analyze the influence of water and soil resources utilization in Yangtze River estuary and the coastal line development on river bed evolution and hydrodynamics variation, on the basis of the result of two large-scale sampling investiga-tion during the dry season of 2012 and 2013, we analyzed the bed material composition, particle size distribution and characteris-tics of particle size in flood and dry season respectively at Chengtong reach of Yangtze River estuary. The result indicated that the particle size in the main channel is thicker than that on the shoal and in the branch;the particle size decreases from upstream to the downstream generally. The major types of bed materials in the main channel area are fine sand and silt sand while the bed materials are sand silt and clayey silt on the shoal and in branch channel area;in 2012, the content of sand is the largest at this reach, followed by silt and clay.