CAJ | 학술논문

2011年2月在珠江口八口门进行了同时段综合水文测验，对测验期间资料进行分析，结果表明：（1）八口门分流比从大至小依次为：磨刀门、虎门、洪奇门、蕉门、崖门、虎跳门、鸡啼门和横门；（2）外海潮波传入河口，磨刀门、鸡啼门高潮位首先出现，而虎门和蕉门最后出现，其时差约为1~2h；磨刀门属于强径流弱潮流河口，相比其他口门涨潮流速偏小，落潮流速偏大；（3）八口门潮周期盐度平均值从大至小依次为：虎门、崖门、磨刀门、虎跳门、横门、蕉门、洪奇门、鸡啼门；（4）虎门、崖门和鸡啼门盐度属于强混合型；磨刀门大潮属于强混合型，小潮处于高度层化型河口；其他4个口门属于中等强度混合类型，其特点为下层盐度大，上层盐度小，大潮时混合强一些，小潮时混合弱一些。
2011년2월재주강구팔구문진행료동시단종합수문측험，대측험기간자료진행분석，결과표명：（1）팔구문분류비종대지소의차위：마도문、호문、홍기문、초문、애문、호도문、계제문화횡문；（2）외해조파전입하구，마도문、계제문고조위수선출현，이호문화초문최후출현，기시차약위1~2h；마도문속우강경류약조류하구，상비기타구문창조류속편소，락조류속편대；（3）팔구문조주기염도평균치종대지소의차위：호문、애문、마도문、호도문、횡문、초문、홍기문、계제문；（4）호문、애문화계제문염도속우강혼합형；마도문대조속우강혼합형，소조처우고도층화형하구；기타4개구문속우중등강도혼합류형，기특점위하층염도대，상층염도소，대조시혼합강일사，소조시혼합약일사。
Large scale hydrological observations in the eight estuaries of the Pearl River were simultaneously carried out in February, 2011. Analysis of the field data showed that:(1) the eight estuaries in descendant order of runoff were: Modaomen, Humen, Hongqimen, Jiaomen, Yamen, Hutiaomen, Jitimen and Hengmen; (2) during tide waves going into the estuaries, Modaomen and Jitimen reached their top water level first, Humen and Jiaomen the last, and their time difference about 1 to 2 hours; the runoff was strong and tide was weak in Modaomen; the flood velocity in Modaomen was smaller than those in other estuaries, but ebb velocity the contrary; (3) the eight estuaries in descendant order of average salinity were: Humen, Yamen, Modaomen, Hutiaomen, Hengmen, Jiaomen, Hongqimen and Jitimen;(4) Humen, Yamen and Jitimen were of strong salinity mixing type;Modaomen belonged to strong salinity mixing type during spring tide, but high-degree stratification type during neap tide. other four estuaries belonged to moderate-degree mixing type, which were characterized by high salinity at bottom layer and low at surface layer, strong mixing during spring tide and weak mixing during neap tide.