LI Xiang, HE Ping, ZHANG Yutao, et al. Charactoristics of Summer Air Anion Concentration in Different Ecological Functional Areas of Southern Edge of Junggar Basin[J]. Bulletin of Soiland Water Conservation, 2015, 35(4): 229-234.
DOI:
LI Xiang, HE Ping, ZHANG Yutao, et al. Charactoristics of Summer Air Anion Concentration in Different Ecological Functional Areas of Southern Edge of Junggar Basin[J]. Bulletin of Soiland Water Conservation, 2015, 35(4): 229-234. DOI: 10.13961/j.cnki.stbctb.2015.04.042.
Charactoristics of Summer Air Anion Concentration in Different Ecological Functional Areas of Southern Edge of Junggar Basin
[Objective] Air anion concentration in different ecological functional zones in southern margin of Junggar Basin was monitored in summer in order to provide a reference for rating regional air quality. [Methods] The concentrations of negative air ion in different ecological function areas (water body
forest area
parking lot
populated districts)by AIC-1000 type instrument. SPSS 17.0 was used for statistical analysis. [Results] (1) The concentrations in different regional areas ranked as: Jinghe > Hami > Tianchi > Baerluke. And the difference between the concentrations of Jinghe and Tianchi and values of Hami and Baerluke was significant (p<0.05); (2) In local ecological function areas
water body and forest area had higher concentration of negative air ions; and the daily concentration showed that it was higher in the morning and evening
and lower in the noon; (3) The rank of air quality levels(CI): Tianchi (level A
1.28±0.42 ind/cm3) > Jinghe (level A
1.16±0.08 ind/cm3) > Hami (level D
0.33±0.14 ind/cm3) > Baerluke (level D
0.32±0.03 ind/cm3); (4) Weather conditions could also influence the concentration of negative air ions
a rank was measured as: rainy(699 ind/cm3) > dust(507 ind/cm3) > sunny(428 ind/cm3) > cloudy(395 ind/cm3). [Conclusion] Changes in air quality and the concentration of negative air ions were basically synchronized in different ecological function areas. Air quality along the southern Junggar Basin showed an inferior-superior-inferior trend graphically form east to west.
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