水利学报
水利學報
수리학보
2014年
4期
394-402
,共9页
黄磊%方红卫%王靖宇%何国建
黃磊%方紅衛%王靖宇%何國建
황뢰%방홍위%왕정우%하국건
河流泥沙%磷迁移%水槽试验
河流泥沙%燐遷移%水槽試驗
하류니사%린천이%수조시험
river sediment%phosphorus transport%flume experiment
水体中磷的迁移转化过程,对于河流生态环境有着至关重要的影响。传统的水质模型缺乏对磷迁移转化过程机理和规律的深入探讨与分析。本文建立河流中水动力-泥沙-磷迁移过程的分相模型,在水流运动与泥沙输移模拟的基础上,从基本的化学反应出发,研究磷在河流中的迁移过程。首先,考虑天然河流中磷的来源及其不同形态,基于泥沙颗粒表面电荷非均匀分布的认识,利用修正后的表面络合模型研究悬移质泥沙对磷的吸附;其次,分析有氧与无氧条件下泥沙颗粒中铁/铝(氢)氧化物的不同形态,以描述磷在活性底泥层中的赋存形式;然后,重点关注河床冲淤变形,分析磷在河床表面的沉积与再释放。最后,本文设计磷水槽试验,分析泥沙颗粒运动对磷迁移的影响,并对模型进行验证。结果表明,泥沙运动对磷迁移有显著影响,磷浓度沿程分布与含沙量间存在较好的线性关系,尤其是溶解相磷;本文建立的模型可以合理地反映磷随着泥沙颗粒的迁移过程。
水體中燐的遷移轉化過程,對于河流生態環境有著至關重要的影響。傳統的水質模型缺乏對燐遷移轉化過程機理和規律的深入探討與分析。本文建立河流中水動力-泥沙-燐遷移過程的分相模型,在水流運動與泥沙輸移模擬的基礎上,從基本的化學反應齣髮,研究燐在河流中的遷移過程。首先,攷慮天然河流中燐的來源及其不同形態,基于泥沙顆粒錶麵電荷非均勻分佈的認識,利用脩正後的錶麵絡閤模型研究懸移質泥沙對燐的吸附;其次,分析有氧與無氧條件下泥沙顆粒中鐵/鋁(氫)氧化物的不同形態,以描述燐在活性底泥層中的賦存形式;然後,重點關註河床遲淤變形,分析燐在河床錶麵的沉積與再釋放。最後,本文設計燐水槽試驗,分析泥沙顆粒運動對燐遷移的影響,併對模型進行驗證。結果錶明,泥沙運動對燐遷移有顯著影響,燐濃度沿程分佈與含沙量間存在較好的線性關繫,尤其是溶解相燐;本文建立的模型可以閤理地反映燐隨著泥沙顆粒的遷移過程。
수체중린적천이전화과정,대우하류생태배경유착지관중요적영향。전통적수질모형결핍대린천이전화과정궤리화규률적심입탐토여분석。본문건립하류중수동력-니사-린천이과정적분상모형,재수류운동여니사수이모의적기출상,종기본적화학반응출발,연구린재하류중적천이과정。수선,고필천연하류중린적래원급기불동형태,기우니사과립표면전하비균균분포적인식,이용수정후적표면락합모형연구현이질니사대린적흡부;기차,분석유양여무양조건하니사과립중철/려(경)양화물적불동형태,이묘술린재활성저니층중적부존형식;연후,중점관주하상충어변형,분석린재하상표면적침적여재석방。최후,본문설계린수조시험,분석니사과립운동대린천이적영향,병대모형진행험증。결과표명,니사운동대린천이유현저영향,린농도연정분포여함사량간존재교호적선성관계,우기시용해상린;본문건립적모형가이합리지반영린수착니사과립적천이과정。
Phosphorus transport in natural water plays a crucial role in ecological environment. Traditional models of water quality mostly simplify such processes into some empirical parameters,without a comprehen-sive understanding of the intrinsic mechanisms. In this paper, a model of hydrodynamic-sediment-phospho-rus transport has been established, in which the chemical and sediment dynamics are integrated to study the phosphorus transport with river sediment. The phosphorus adsorption by sediment is considered using the modified surface complexation modeling based on the heterogenous surface charge distribution of natural sediment. In addition, the aerobic layer and anaerobic layer are distinguished to study the distribution of phosphorus between dissolved phase and particulate phase in the active sediment layer. Furthermore,the riv-erbed deformation is introduced to analyze the deposition and release of phosphorus at the bed surface. A flume experiment is designed to study the effects of sediment on phosphorus transport and validate the mod-el. The results show that the phosphorus concentration is linearly correlated with sediment concentration, and the proposed model can reasonably reflect the phosphorus transport with sediment.