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471.
A. Sundaram K.M.S. Sundaram 《Journal of environmental science and health. Part. B》2013,48(5):1119-1154
Abstract The effect of sunlight radiation, rainfall and droplet spectra of sprays on per ‐sistence of a Bacillus thuringiensis subspp. kurstaki (Btk) formulation, DiPel® 76AF, was examined after application onto spruce [Picea glauca (Moench) Voss] foliage. The investigation consisted of three studies: (i) Study I: a laboratory microcosm study to examine the photostability of DiPel 76AF deposits on foliage after different periods of exposure to two radiation intensities, (ii) Study II: a laboratory microcosm study to examine the rainfastness of foliar deposits after exposure to different amounts of rainfall consisting of two separate droplet spectra, and (iii) Study III: a field microcosm study to investigate the influence of two different droplet spectra of DiPel 76AF sprays on foliar persistence of Btk under natural weathering conditions. In all studies, persistence of Btk was investigated both by bioassay [using spruce budworm (Choristoneura fumiferana Clemens)] and total protein assay. The findings of Study I indicated that bioactivity of foliar deposits decreased with increasing duration of exposure to radiation, and with increasing radiation intensity. The half‐life (DT50, the exposure period required for 50% of the initial bioactivity to disappear) was 5.1 d for the low intensity, and 3.9 d for the higher intensity. In contrast with the bioassay results, the total protein levels [determined by the bicinchoninic acid (BCA) method] showed no decrease with increasing duration of exposure, or with increasing radiation intensity. The findings of Study II indicated that bioactivity of foliar deposits decreased with increasing cumulative rainfall. A new term, RF50 [the amount of rain (in mm) required to washoff 50% of the initial deposit], was introduced to understand the relationship between rainfall intensity and reduction in bioactivity. When the same amount of rain was applied in different droplet sizes, the RF50 value was high (5.2 mm) for the small rain droplets, and was low (2.9 mm) for the large rain droplets. Similar to the bioassay results, the total protein concentrations (determined by the BCA method) decreased with increasing amount of rain and with increasing rainfall intensity. The RF50 value (obtained using ng protein /cm2) was 5.4 mm for the small rain droplets, and was 3.4 mm for the large rain droplets. The field microcosm study indicated that when DiPel 76AF was applied in small droplets (Dv.5 of 65 μm), the persistence of bioactivity was ca 8.0 d, whereas when it was applied in large droplets (Dv.5 of 130 nm) it was ca 11 d. Bioactivity decreased with time after spray, and the DT50 was 1.98 d for the spray of small droplets, and 2.87 d for that of large droplets. Similar to the bioactivity, the total protein concentrations also decreased with time after spray, and the DT50 values for the small and large droplet spectra were 3.45 and 6.07 d respectively. 相似文献
472.
酸雨对水稻、小麦和油菜种子萌发的影响 总被引:24,自引:3,他引:21
采用pH2.0、2.5、3.0、3.5、4.0与5.0模拟酸雨处理水稻、小麦和油菜种子的实验结果表明,3者在pH 2.0时不发芽,在pH 2.5时只有水稻和小麦异状发芽,pH≥3.0时,水稻、小麦和油菜种子的发芽率、发芽势、发芽指数、活力指数都与pH值显著正相关,水稻和小麦的异状发芽率则随pH值上升而降低.部分生理指标的实验结果表明,水稻、小麦和油菜的吸水值、呼吸速率和贮藏物质运转效率也与pH值显著正相关,水稻与小麦贮藏物质消耗率与pH值显著正相关,而油菜与pH值显著负相关;水稻、小麦和油菜的芽、根长抑制指数都与pH值显著负相关.酸雨胁迫下,种子各项指标变幅为水稻<小麦<油菜,这表明抗酸雨胁迫能力为水稻>小麦>油菜. 相似文献
473.
依据山东省多年来的降水观测资料,评价了酸雨污染现状,研究了酸雨时空分布规律.通过对主要酸雨前体物的排放强度与降水酸度的关系,土壤酸碱性与降水酸度的关系,以及气象条件对酸雨影响的分析,探讨了山东省酸雨的成因. 相似文献
474.
On East Asian Sand and Duststorms and Associated Significant Dustfall Observed from January to May 2001 总被引:4,自引:0,他引:4
Monitoring of dust pollution at the western shore of Tae-ahn Peninsula (TAP) and in the Chongju area of central Korea was carried out from January to May 2001. It was found that in Koreathere were 9 cases of sand and duststorms (DS) and 16 associatedsignificant dustfall (SD) days. Observed maximum concentrations of DS and SD coming from NW China and Mongolia were in the rangeof 300–920 for TSP, 200–690 for PM10 and 100–170 g m-3 for PM2.5.Satellite measurements clearly showed the formation and subsequent movement of DS to the Korean Peninsula and onward to the Korea East Sea, Japan and the Gulf of Alaska. According to satellite image analysis of dust clouds there were abundant coarse particles, measuring in size of 11.0 m. Medium-sizedparticles measuring in the range of 3.5–7.0 were also prevalent,while fine particles of less than 2.0 m were less distinctive in reflectivity. Measured values of PM2.5 were alsorelatively low with SD events.The measured average pH values of dusty precipitation associatedwith DS were 7.24. Alkaline precipitation can play a `temporary'role in the neutralization of acidified soil until the subsequentevent of acidic rain. The new selection criteria of SD days from PM2.5 at 85 g m-3, PM10 190 g m-3 and TSP 250 g m-3 are recommended on dust pollution occurring from the invasion of a DS elsewhere. 相似文献
475.
ABSTRACT: Catch in standard (unshielded) rain gages exposed 3 feet above the land surface was compared with catch in pit (buried) gages exposed 1 inch above the land surface. These tests confirmed that catch in standard gages under estimates point rainfall in forest openings, as well as in conventional weather stations. Pit gages caught significantly (P=0.05) more rain than did standard gages at each of four locations tested. Catch increases ranged from 2.3 to 3.4 percent. 相似文献
476.
477.
利用全国多雨、中雨和少雨典型区的自记雨量曲线和 Kinnel 方程:E=29.233·(1-e~(-(0.0477I+0.112)))计算出各点各次降雨的雨能值,并作出各区按月降雨(x)和雨能(y)的关系式:y=15.592x-171.630(多雨区),y=16.257x-280.279(中雨区),y=16.493x-107.676(少雨区)。将全国77个观测点的按月雨量资料计算出全年的雨能值。通过作图得到我国多雨和中雨区的年降雨量 P 和年雨能值 E 的关系:E=11.67p;和少雨区的关系:E=14.95P。从而可用此来估算全国各测点的雨能值。 相似文献
478.
479.
480.
Ian D. Moore 《Journal of the American Water Resources Association》1983,19(6):961-965
ABSTRACT: Precipitation, throughfall, and stream pH were measured weekly over a 27-week period in 1982 on the Little Millseat watershed in eastern Kentucky. The average pH values over the study period were 4.3, 4.9, and 6.4, respectively, indicating significant buffering as water moved from the atmosphere, through the deciduous canopy, and through or over the soil to the stream. Regression analysis demonstrated that the timing and amount of precipitation were important factors influencing the pH of the throughfall. Weekly precipitation and the three-week average precipitation were statistically significant variables, explaining 53 percent of the variance in the observed through- fall pH. Precipitation pH was not a statistically significant variable for this watershed and sampling period. 相似文献