生态环境学报
生態環境學報
생태배경학보
ECOLOGY AND ENVIRONMENT
2014年
12期
1933-1937
,共5页
王明仕%李晗%王明娅%曹宁%宋党育
王明仕%李晗%王明婭%曹寧%宋黨育
왕명사%리함%왕명아%조저%송당육
中国%大气降尘%降尘量%沙尘暴
中國%大氣降塵%降塵量%沙塵暴
중국%대기강진%강진량%사진폭
China%dust fall%content%sandstorm
为了研究中国大气降尘量的地域性分布特征,探讨大气降尘的影响因素,文章以中国大气降尘研究为基础,汇总近20年25个行政区44个地区的降尘量数据,以10 t·km-2·month-1为间隔首次划分降尘区间,为中国降尘量标准的制定提供参考。中国大气降尘现有研究多集中在东北部、中东部地区以及西北沙漠地区,降尘量整体分布为北方高于南方,西部多于东部。除涉及强沙尘暴袭击区域外,现有研究区域的降尘量算术平均值为14.73 t·km-2·month-1,53.7%的研究区域降尘量小于该平均值。降尘量少于20 t·km-2·month-1的地区多集中于沿海地区、长江中下游地区以及东北平原地区,此类地区多为旅游景区和重要的商品粮产地,植被覆盖率较高,水土保持性能良好,且不易有较大的风沙侵袭;华北平原地区、内蒙古高原地区和准噶尔盆地一带降尘量相对偏高,此类区域多为重工业区,发展经济的同时造成了不同程度的环境污染和资源掠夺;降尘量最大的地区位于塔里木盆地一带,最大值为2915.96 t·km-2·month-1,属于沙尘暴多发区。大气降尘量虽会在一定程度上受到经济发展、工业布局、能源结构的影响,但更多的是因为其地域性差异而造成降尘量不同。中国现有的各地降尘量的数据较少,且研究区多位于城市等人类活动中心,更多地区的降尘量尚需要进一步研究。
為瞭研究中國大氣降塵量的地域性分佈特徵,探討大氣降塵的影響因素,文章以中國大氣降塵研究為基礎,彙總近20年25箇行政區44箇地區的降塵量數據,以10 t·km-2·month-1為間隔首次劃分降塵區間,為中國降塵量標準的製定提供參攷。中國大氣降塵現有研究多集中在東北部、中東部地區以及西北沙漠地區,降塵量整體分佈為北方高于南方,西部多于東部。除涉及彊沙塵暴襲擊區域外,現有研究區域的降塵量算術平均值為14.73 t·km-2·month-1,53.7%的研究區域降塵量小于該平均值。降塵量少于20 t·km-2·month-1的地區多集中于沿海地區、長江中下遊地區以及東北平原地區,此類地區多為旅遊景區和重要的商品糧產地,植被覆蓋率較高,水土保持性能良好,且不易有較大的風沙侵襲;華北平原地區、內矇古高原地區和準噶爾盆地一帶降塵量相對偏高,此類區域多為重工業區,髮展經濟的同時造成瞭不同程度的環境汙染和資源掠奪;降塵量最大的地區位于塔裏木盆地一帶,最大值為2915.96 t·km-2·month-1,屬于沙塵暴多髮區。大氣降塵量雖會在一定程度上受到經濟髮展、工業佈跼、能源結構的影響,但更多的是因為其地域性差異而造成降塵量不同。中國現有的各地降塵量的數據較少,且研究區多位于城市等人類活動中心,更多地區的降塵量尚需要進一步研究。
위료연구중국대기강진량적지역성분포특정,탐토대기강진적영향인소,문장이중국대기강진연구위기출,회총근20년25개행정구44개지구적강진량수거,이10 t·km-2·month-1위간격수차화분강진구간,위중국강진량표준적제정제공삼고。중국대기강진현유연구다집중재동북부、중동부지구이급서북사막지구,강진량정체분포위북방고우남방,서부다우동부。제섭급강사진폭습격구역외,현유연구구역적강진량산술평균치위14.73 t·km-2·month-1,53.7%적연구구역강진량소우해평균치。강진량소우20 t·km-2·month-1적지구다집중우연해지구、장강중하유지구이급동북평원지구,차류지구다위여유경구화중요적상품량산지,식피복개솔교고,수토보지성능량호,차불역유교대적풍사침습;화북평원지구、내몽고고원지구화준갈이분지일대강진량상대편고,차류구역다위중공업구,발전경제적동시조성료불동정도적배경오염화자원략탈;강진량최대적지구위우탑리목분지일대,최대치위2915.96 t·km-2·month-1,속우사진폭다발구。대기강진량수회재일정정도상수도경제발전、공업포국、능원결구적영향,단경다적시인위기지역성차이이조성강진량불동。중국현유적각지강진량적수거교소,차연구구다위우성시등인류활동중심,경다지구적강진량상수요진일보연구。
In order to elucidate the distribution characteristics and influence factors of dust fall in China, 44 dust fall contents of 25 administrative regions in the recent 20 years summarized. For the first time, China was divided into dust fall regions at 10 t·km-2·month-1 interval. Current researches on dust fall in China focused on the northeast, east midlands and northwest desert area. In general, dustfall in the south was higher than that in the north, and the west higher than the east. Except the strong sandstorm areas, the arithmetic mean value of dust fall in the existing research areas was 14.73 t·km-2·month-1, with 53.7% of the research area less than the average. The dust fall less than 20 t·km-2·month-1 was mainly loctaed in the coastal areas, the middle and lower reaches of the Yangtze river region and the northeast plain. Such areas are tourism areas or important commodity grain producing areas, with high vegetation coverage rate, good water and soil conservation performance, and seldom sand invasion. The regions with heavy dust fall included the north China plain area, Inner Mongolia plateau and Junggar basin. These regions are heavily industrialized, with environment polluted and resources over exploited. The highest dust fall, with a maximum value of 2915.96 t·km-2·month-1, was found in the sandstorm prevailing Tarim basin. The huge difference in dust fall is mainly determined by regional difference, and to a less extent affected by economic development, industrial layout and energy structure. . The areas currently studied in terms of dust fall are mainly located in cities, i.e. centers of human activities, leaving many regions untouched, which need to be studied in the future.