姚江

摘要： 姚江主源为梁弄溪,发源于四明山夏家岭东北眠冈山西坡,主峰海拔687m。自源头至姚江与奉化江汇合处,河长102.4km(原河长记载为107.4km,杭甬运河建设裁弯取直河长减少5km),余姚境内河长70km。姚江干流河道比降平缓,其中大厍船闸至通明闸,河长13.1km,河道平均比降五千分之一;通明闸至姚江大闸,河长82.6km,河道平均比降十万分之一。姚江流域内2014年末总人口313.8万人,其中绍兴上虞区78万人,宁波余姚市83.7万人,宁波慈溪市104.6万人,宁波江北区24.3万人,宁波镇海区23.2万人。姚江流域内2014年末地区生产总值3549亿元,其中绍兴上虞区681亿元,宁波余姚市808亿元,宁波慈溪市1112亿元,宁波江北区303亿元,宁波镇海区646亿元。东排入甬江流域(面积1878km^2)主要涉及上虞区、余姚市、宁波的江北区、镇海区,至2014年末,流域内人口约120万人,地区生产总值约1180亿元。

摘要： Deposits of an extrordinary flood that took place in October 2013 in the lower Yaojiang River were systematically collected. Then grain size analysis and magnetic measurement were conducted to study the characteristics of grain size and magnetic properties in relation to the flood dynamics. The results showed that the flood sediments were composed mainly of silts (58.72%),clay(about 23.27%) and fine sand (18.01%),or could be named as clay-sandy silt. The grain size of the de-posits respectively from low flat,high flat and flood plain showed a gentle finer trend or with little difference. The frequency curve of grain-size had twin peaks or multimodal peak,and positive bias. The probability cumulative curves were relatively flat and all of them had two-stage. Magnetic parameters showed that the magnetic minerals in the flood sediment were mainly composed of ferri magnetic minerals. The high values of χARM in the sediments from the two branch streams (Lanshu and Houqing) in the downtown and the lower stream out of the town indicated a relative higher concentration of ferri magnetic minerals,reflecting the sediments getting finer or more local materials. Through correlation of the grain-size composition with some other fine deposits formed in different sedimentary environment,it indicated that the deposits was much similar to that from Jiaxing (another flood deposit formed in the same time),and also similar to the "yellow silt″ collected from the area of the ancient Liangzhu city near Hangzhou, but different quite a lot from the intertidal sediments from Hangzhou Bay.%2013年10月受"菲特"台风的影响,浙江余姚境内的姚江流域发生了特大洪水.通过系统采集不同河段高﹑低河漫滩及泛滥平原的沉积物样品,开展粒度分析和磁性测量,探讨了该地区特大洪水事件在沉积物粒度及磁性参数方面的表征特征.研究表明,沉积物粒度组成以粉沙为主﹝平均58.72%),黏土次之﹝23.27%),沙最少﹝18.01%),主体成分为黏土-沙质粉沙;从低河漫滩﹑高河漫滩到泛滥平原,沉积物粒度具有变细趋势,但差别不大;频率曲线表现为较宽的单峰,略显正偏;概率累积曲线较为平缓且均为两段式.入城段与城区干流段沉积物中磁性参数χ、SIRM呈现高度的相关性,表明磁性矿物主要由亚铁磁性矿物组成,较高的χARM表明沉积物中含有较多的稳定单畴亚铁磁性矿物.区域横向对比结果表明,余姚洪水沉积物在粒度结构上可与同时期形成的嘉兴地区的洪水沉积物作比较,也与良渚古城附近﹑杭州平原广泛发育的"黄粉土"相近,而与杭州湾高潮滩沉积物明显不同.

摘要： 沉思姚江畔 从河姆渡展馆出来，伫立于姚江畔，凝望着古老而神圣的遗址，我的思绪犹如那江水，汹涌翻腾不息。徜徉于悠远的历史长河，寻觅着耀眼的智慧火花，不由为先民的睿智所折服，为华夏的璀璨而自豪。

摘要： 宁波是海上丝绸之路的起点之一，也是“一带一路”沿线重要的现代化港口城市。在“一带一路”国家发展战略的背景下，宁波市委市政府提出打造“一都三城”（东亚文化之都、影视之城、音乐之城、书香之城）的战略目标，把宁波音乐港建设作为“音乐之城”建设的最要抓手，写入市委第十二届十一次全会报告，作为当前文化建设的主攻方向之一，以音乐为纽带，加速融入21世纪海上丝绸之路国家发展战略。

摘要： 起源于18世纪上叶的姚剧,属吴语系滩簧类地方剧种,以其传统剧目丰富、表演通俗易懂、剧目贴近生活而深受百姓欢迎。新中国成立后,姚剧在经历改革后焕发新的生机：1956年,余姚姚剧团成立;2008年,姚剧入选第二批国家级非物质文化遗产名录;2012年剧团改制,余姚市姚剧保护传承中心成立……

摘要： 浙东余姚，人文发祥之地。清澈的姚江，滚滚东去，回荡着河姆渡先民的歌声。余姚城中有龙泉山，山有中天阁。深秋的暮霭里，这座简朴的建筑显得格外沉静而又安详。游人喜直扑山顶，往往在中天阁侧拾级而上，倘若稍停半步，左转入小门，便入中天阁，那该多好啊!进入中天阁，你的目光就会牢牢吸附于阁中布展的文字与图片上——王阳明、姚江书院、龙山书院……一系列著名人物与文化事实扑面而来。

摘要： 为了缓解水资源供需矛盾，曹娥江至宁波引水（引曹南线）工程建成之前，利用已建成的曹娥江至慈溪引水工程（引曹北线）在干旱期间对宁波应急引水，是宁波市当前急需解决的重要课题。在对引曹北线工程挖潜方案等前期研究的基础上，通过分析姚江历年水文情况、查清引水线路相关河道及闸站的管理现状、与相关部门座谈等方式，最后提出切实可行的曹娥江至宁波应急引水方案。

摘要： 一江春水那一年我的故乡被一场洪水冲走冲到了清水江的彼岸静静地溶化了乡愁的距离