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中国沙漠 ›› 1992, Vol. 12 ›› Issue (2): 27-33.

• 论文 • 上一篇    下一篇

北京地区风沙活动的监测

贺大良   

  1. 北京风沙整治研究试验站
  • 出版日期:1992-06-20 发布日期:1992-06-20

Wind-sand Activity Monitoring in Beijing Region

He Daliang   

  1. Institute of Desert Research, Academia Sinica, Lanzhou
  • Online:1992-06-20 Published:1992-06-20

摘要: 1990-1991年北京风沙整治研究试验站又对北京市东南部沙质土壤地区做了风沙活动的监测,以判断近五年来沙荒地改造利用的效果。监测结果表明:1、北京地区风沙日数继续下降,由1981-1985年的平均每年19.8次下降为1986-1990年的12.4次。扬沙天气日数有所增加,由1951-1985年平均占71.6%,增加为1986-1990年的77.4%。今后防治的重点仍应以防治本地沙源为主,风沙日数下降与当地植被覆盖增加相关。2、风沙天气日数/大风天气日数的比值由前35年的1.40下降为近5年的0.82,说明近五年的防治风沙是有成绩的,风沙日数的减少不单纯是因为大风日数减少所致。3、对典型地段起沙量的观测表明:同样风速下的起沙量大幅度降低,原因是植被保护增加和耕作面形成土壤结壳。4、对沙壤质农田的降尘进行了连续观测,1990年4月-1991年3月年降尘总量267.9 吨/平方公里.年,月平均降尘22.31 吨/平方公里.月,此值略大于北京全市平均值。对今后风沙的防治也提出了原则意见。

关键词: 北京地区, 风沙活动, 监测, 风沙天气, 沙尘暴, 扬沙, 浮尘, Q-V图

Abstract: Following two-year survey from 1985 to 1986,the Beijiang Wind-sand control experiment station conducted monitoring of wing-sand activities in sandy soil areas of southeastern Berjing.The monitoring resuits show that:1.The number of days with wind-sand is continuously decreasing,e.g,the annual mean number of days with wind-sand decreased from 19.8 in 1981-1985 to 12.4 in 1986-1990.2.The sand of wind-sand activities mainly come from local origin,therefore,we must put priority on local sand control sand control in the comming years.In 1951-1985 the number of bloqing sand days occupied 71.6%,while in 1986-1990 this value reached up to 77.4%.3.The ratio between the number of days with wind-sand and the number of days with gale reduced from 1.40 in the past 35 years to 0.82 in recent 5 years.4.The results observated in typical areas show that under the same wind velocity the blowing sand amount greatly reduced due to increasing vegetation cover and soil crust fromed on cultivated sruface.5.Obserbation results in sandy loam fields showed that the total dustfall deposition rate from April of 1990 to March of 1991 was 267.9 T/km2.yr,monthy averaged 22.31 T/km2,i.e.slightly higher than the mean value in urban area of Beijing.