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Tayyab Muhammad Yang Ziqi Zhang Caifang Islam Waqar Lin Wenxiong Zhang Hua 《Environmental science and pollution research international》2021,28(35):48080-48096
Environmental Science and Pollution Research - Sugarcane monoculture (SM) often leads to soil problems, like soil acidification, degradation, and soil-borne diseases, which ultimately pose a... 相似文献
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广州近地面臭氧浓度特征及气象影响分析 总被引:10,自引:0,他引:10
利用2015年广州市近地面逐时臭氧(O_3)观测资料及气象数据,分析了广州地区近地面的O_3浓度时空分布特征及其与气象因子的关系.结果表明:广州地区城郊的O_3浓度高于中心城区;广州地区近地面的O_3浓度超标时间主要出现在4—9月,8月O_3浓度最高,3月O_3浓度最低;O_3浓度日变化呈现"单峰型"分布,早上7:00—8:00出现最低值,15:00达到峰值;O_3浓度与气温呈正相关,当气温高于30℃时,O_3浓度随温度升高增加明显;与相对湿度呈负相关,当相对湿度大于60%时,O_3浓度显著降低;当气压小于1010 hpa时,与气压呈负相关,当气压大于1010 hpa时,与气压呈正相关;当风力为2~3级吹西北偏西至西南偏西风区间时,O_3浓度最高,说明广州偏西部可能存在O_3污染源区;O_3浓度在晴天最高,其次是少云和多云天气,最低是在雨天.总体而言,气温高、日照长、辐射强、气压低、湿度小及2~3级的风力是广州地区近地面产生高浓度O_3的主要气象因素.当广州O_3浓度出现超标时,气温变化范围为25.9~37.4℃,相对湿度变化范围为29%~83%,气压变化范围为989.4~1009.1 h Pa,风速变化范围为0.7~5.8 m·s~(-1),紫外辐射强度日最大1 h均值最小为32.6 W·m~(-2),10:00—14:00均值最小为27.3 W·m~(-2). 相似文献
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Ziqi Zhao Meng Li Wansong Huang Nuowei Guo Qian Zhang 《Frontiers of Environmental Science & Engineering》2023,17(6):75
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Xiaolan Li Guiqian Tang Liguang Li Weijun Quan Yangfeng Wang Ziqi Zhao Ningwei Liu Ye Hong Yanjun Ma 《环境科学学报(英文版)》2022,34(3):300-310
Visibility observed at different altitudes is favorable to understand the causes of air pollution. We conducted 4-years of observations of visibility at 2.8 and 60 m and particulate matter(PM) concentrations from 2015 to 2018 in Shenyang, a provincial city in Northeast China. The results indicated that visibility increased with the increasing height in winter(especially at night), and decreased with height in summer(especially at the daytime). PM concentration exhibited opposite vertical variati... 相似文献
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为避免或减轻工程结构在建造和运营期间因结构振动产生不同程度损伤,造成安全隐患危及人们生命财产安全,针对结构振动损伤识别技术展开研究,探讨不同深度学习方法发展情况及其利弊,寻找更具可行性的损伤识别方法,并对其最新研究及应用现状进行全面综述。研究结果表明:应用深度学习开发新的结构损伤识别技术,无需冗余的数据预处理以及手工提取损伤特征,实现以较高精度实现损伤识别任务;一维卷积神经网络(1D-CNN)以其独特的应用优势,在数据样本有限条件下较二维卷积神经网络(2D-CNN)表现更为出色。研究结果可为数据驱动的结构损伤识别问题提供新思路,进一步完善土木结构健康监测研究体系。 相似文献
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近年来,随着中国经济的快速发展,水体中氨氮超标问题已严重影响到人类身体健康和生态环境平衡,有效去除水体中的氨氮已成为人们研究的热点.在传统污水生物脱氮处理中,常采用微生物的硝化、反硝化作用去除污水中的氮素,从而降低对环境的污染.本文从活性污泥反应器中分离出一株异养硝化-好氧反硝化菌株,并命名为X1-L.菌体经形态学观察、生理生化测定及16S rRNA基因序列分析,确定属于芽孢杆菌属(Bacillus sp.),Genbank登录号为MT457091,并利用MEGA7.0软件建立了相应的系统发育树.在以NH4+-N为唯一氮源的条件下,菌株X1-L生长较好,COD去除率为96.4%,氨氮去除率达到99.6%,经硝化作用去除的氮有43.7%,证明菌株X1-L具有异养硝化能力.在以NO2--N或NO3--N为唯一氮源的条件下,菌株X1-L生长也较好,COD去除率分别为95.3%和96.4%,NO2--N和NO3--N去除率分别为95.5%和96.5%,经反硝化作用去除的氮分别有67.7%和68.2%,证明菌株X1-L具有好氧反硝化能力. 相似文献
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为探究大温差地区曲线梁桥在近断层脉冲型地震动作用下的地震响应和碰撞效应,以西北大温差地区某曲线连续梁桥为工程实例,建立全桥非线性有限元模型并考虑变温作用对支座刚度的影响;分别以桥墩内力、支座位移和邻梁碰撞效应为指标研究曲线梁桥在近断层脉冲型地震动作用下的地震反应特性。结果表明:温度越低,地震波作用于结构的内力响应越大;曲线梁桥在地震动作用下邻梁间碰撞为面-面碰撞,且温度越高,碰撞效应越强;高阻尼橡胶支座在低温下体现出较强的耗能能力,在大温差地区的桥梁抗震设计中可作为参考;近断层脉冲地震动相较于远场地震动,结构地震响应更大,对结构的破环性更强,故在近断层地区的桥梁抗震设计中应予以重视。 相似文献
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Dongyou Wu Tenglong Shi Xiaoying Niu Ziqi Chen Jiecan Cui Yang Chen Xueying Zhang Jun Liu Mingxia Ji Xin Wang Wei Pu 《环境科学学报(英文版)》2022,34(4):53-65
The Asian Tropopause Aerosols Layer (ATAL) refers to an accumulation of aerosols in the upper troposphere and lower stratosphere during boreal summer over Asia, which has a fundamental impact on the monsoon system and climate change. In this study, we primarily analyze the seasonal to sub-seasonal variations of the ATAL and the factors potentially influencing those variations based on MERRA2 reanalysis. The ability of the reanalysis to reproduce the ATAL is well validated by CALIPSO observations from May to October 2016. The results reveal that the ATAL has a synchronous spatiotemporal pattern with the development and movement of the Asian Summer Monsoon. Significant enhancement of ATAL intensity is found during the prevailing monsoon period of July–August, with two maxima centered over South Asia and the Arabian Peninsula. Owing to the fluctuations of deep convection, the ATAL shows an episodic variation on a timescale of 7–12 days. Attribution analysis indicates that deep convection dominates the variability of the ATAL with a contribution of 62.7%, followed by a contribution of 36.6% from surface pollutants. The impact of precipitation is limited. The ATAL further shows a clear diurnal variation: the peak of ATAL intensity occurs from 17:30 to 23:30 local time (LT), when the deep convection becomes strongest; the minimum ATAL intensity occurs around 8:30 LT owing to the weakened deep convection and photochemical reactions in clouds. The aerosol components of the ATAL show different spatiotemporal patterns and imply that black carbon and organic carbon come mainly from India, whereas sulfate comes mainly from China during the prevailing monsoon period. 相似文献