热带地理
熱帶地理
열대지리
TROPICAL GEOGRAPHY
2015年
1期
13-20
,共8页
徐丹%邓孺孺%陈启东%秦雁%梁业恒
徐丹%鄧孺孺%陳啟東%秦雁%樑業恆
서단%산유유%진계동%진안%량업항
气溶胶粒子谱%CE318太阳分光光度计%消光法%广州市
氣溶膠粒子譜%CE318太暘分光光度計%消光法%廣州市
기용효입자보%CE318태양분광광도계%소광법%엄주시
aerosol size distribution%CE318%extinction method%Guangzhou
基于CE318太阳光度计观测数据,采用消光法对广州市2011年全年的气溶胶粒子体积浓度、数浓度、体积谱、数浓度谱的全年总体特征,季节性特征及日变化进行了分析。结果表明:1)广州市气溶胶粒子体积浓度年均值为0.45μm3/μm2,春季最高,夏季最低;且粒子体积浓度与浑浊度的相关系数达到0.956。2)广州市气溶胶体积谱为双峰型,数浓度谱为单峰型。半径<0.1μm的细粒子为气溶胶主控粒子,主要由水溶性粒子和煤烟组成。3)广州市的气溶胶污染主要与工业、交通等人为污染有关;其主要成分为水溶性粒子和煤烟,此外还存在少量的沙尘和海洋气溶胶粒子。4)一天当中气溶胶粒子体积浓度随着人类活动增加逐步上升,T 12:00―15:00时段细粒子的体积浓度为一天中最高。
基于CE318太暘光度計觀測數據,採用消光法對廣州市2011年全年的氣溶膠粒子體積濃度、數濃度、體積譜、數濃度譜的全年總體特徵,季節性特徵及日變化進行瞭分析。結果錶明:1)廣州市氣溶膠粒子體積濃度年均值為0.45μm3/μm2,春季最高,夏季最低;且粒子體積濃度與渾濁度的相關繫數達到0.956。2)廣州市氣溶膠體積譜為雙峰型,數濃度譜為單峰型。半徑<0.1μm的細粒子為氣溶膠主控粒子,主要由水溶性粒子和煤煙組成。3)廣州市的氣溶膠汙染主要與工業、交通等人為汙染有關;其主要成分為水溶性粒子和煤煙,此外還存在少量的沙塵和海洋氣溶膠粒子。4)一天噹中氣溶膠粒子體積濃度隨著人類活動增加逐步上升,T 12:00―15:00時段細粒子的體積濃度為一天中最高。
기우CE318태양광도계관측수거,채용소광법대엄주시2011년전년적기용효입자체적농도、수농도、체적보、수농도보적전년총체특정,계절성특정급일변화진행료분석。결과표명:1)엄주시기용효입자체적농도년균치위0.45μm3/μm2,춘계최고,하계최저;차입자체적농도여혼탁도적상관계수체도0.956。2)엄주시기용효체적보위쌍봉형,수농도보위단봉형。반경<0.1μm적세입자위기용효주공입자,주요유수용성입자화매연조성。3)엄주시적기용효오염주요여공업、교통등인위오염유관;기주요성분위수용성입자화매연,차외환존재소량적사진화해양기용효입자。4)일천당중기용효입자체적농도수착인류활동증가축보상승,T 12:00―15:00시단세입자적체적농도위일천중최고。
A CE318 automatic sun tracking spectrophotometer was used to measure direct solar radiation at Guangzhou in 2011. The volume concentration, number concentration, volume distribution, number distribution were inverted, of which the annual and seasonal characteristics and the diurnal variation were studied. The results show that:1) The volume concentration of aerosol at Guangzhou varied seasonally, with a spring maximum and a summer minimum, and the average value of the concentration in 2011 was 0.45 μm3/μm2. The correlation coefficient between volume concentration and turbidity was 0.956. 2) The volume distribution was in a bimodal pattern, while number distribution in a unimodal pattern. Fine particles whose radiuses within 0.1μm were the principle aerosol particles, composed of water dissoluble particles and soot, the main source of which were traffic pollution and industrial pollution. 3) With soluble particles and soot as major composition, and a small number of sand and marine aerosol particles besides, aerosol pollution at Guangzhou was mainly relevant to man-made pollution, such as industrial pollution and traffic pollution. 4) The diurnal variation of particle concentration at Guangzhou was consistent with that of human activities, rising with the increasing of human activities. The concentration of fine particles at the period from 12 o’clock to 15 o’clock increased because of the strong solar radiation.