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81.
合成了一种高吸附容量的磁性生物炭负载Mg-Fe水滑石复合材料(L-BC),并用于去除水中的Cd2+和Ni2+。表征结果表明,采用浸渍联合热解法成功制备了磁性生物炭(M-BC),水热合成法成功地将Mg-Fe水滑石负载在M-BC上。动力学研究结果表明,Cd2+和Ni2+吸附符合伪二级动力学模型,化学吸附为速率控制步骤。等温吸附研究结果表明,L-BC对Cd2+和Ni2+的吸附符合Langmuir模型,为单分子层化学吸附,最大吸附量分别为263.156 mg/g和43.291 mg/g。吸附机理主要为Mg-Fe水滑石层间CO32-和表面羟基与Cd2+和Ni2+产生表面共沉淀。L-BC具有良好的吸附和重复利用性能,是一种很有前景的去除Cd2+和Ni2+的吸附材料。 相似文献
82.
Andrea Emili Alessandro Acquavita Stefano Covelli Lucia Spada Antonella Di Leo Santina Giandomenico Nicola Cardellicchio 《Environmental science and pollution research international》2016,23(13):12582-12595
In situ benthic flux experiments were conducted at two stations in the Mar Piccolo of Taranto (Italy), one of the most industrialised and contaminated coastal areas of the Mediterranean. Sediments of the two stations are notably different in their trace metal content, with a station closer to a Navy harbour showing higher mean concentrations of almost all investigated metals (Al, As, Cd, Cr, Cu, Fe, Hg, Mn, Ni, Pb, V and Zn). Conversely, both stations are characterised by significant Hg contamination, compared to the local baseline. Results of a sequential extraction scheme on surface sediments suggest a relatively scarce mobility of the examined metals (Zn > Ni > Cr > As > Cu > Pb). A Hg-specific extraction procedure showed that most of the element (93.1 %) occurs in a fraction comprising Hg bound to Fe/Mn oxi-hydroxides. Reduction of these oxides may affect Hg remobilisation and redistribution. Porewater profiles of dissolved trace metals were quite similar in the two sites, although significant differences could be observed for Al, Cu, Fe and Hg. The highest diffusive fluxes were observed for As, Fe and Mn. Mobility rates of several trace elements (Al, As, Cd, Cr, Cu, Fe, Hg, Mn, Ni, Pb, V and Zn) were directly measured at the sediment–water interface. Results from benthic in situ incubation experiments showed increasing dissolved metal concentrations with time, resulting in higher fluxes for Cu, Fe, Hg, V and Zn in the most contaminated site. Conversely, fluxes of Mn, Ni and Pb were comparable between the two stations. The estimated flux of Hg (97 μg m?2 day?1) was the highest observed among similar experiments conducted in other highly contaminated Mediterranean coastal environments. Benthic fluxes could be partially explained by considering rates of organic matter remineralisation, dissolution of Fe/Mn oxy-hydroxides and metal speciation in sediments. Seasonal and spatial variation of biogeochemical parameters can influence metal remobilisation in the Mar Piccolo area. In particular, metals could be promptly remobilised as a consequence of oxygen depletion, posing a serious concern for the widespread fishing and mussel farming activities in the area. 相似文献
83.
Nitrogen enrichment in runoff sediments as affected by soil texture in Beijing mountain area 总被引:3,自引:0,他引:3
Yang Yang Zhihan Ye Baoyuan Liu Xianqin Zeng Suhua Fu Bingjun Lu 《Environmental monitoring and assessment》2014,186(2):971-978
Enrichment ratio (ER) is widely used in nonpoint source pollution models to estimate the nutrient loss associated with soil erosion. The objective of this study was to determine the ER of total nitrogen (ERN) in the sediments eroded from the typical soils with varying soil textures in Beijing mountain area. Each of the four soils was packed into a 40 by 30 by 15 cm soil pan and received 40-min simulated rainfalls at the intensity of 90 mm h?1 on five slopes. ERN for most sediments were above unity, indicating the common occurrence of nitrogen enrichment accompanied with soil erosion in Beijing mountain area. Soil texture was not the only factor that influenced N enrichment in this experiment since the ERN for the two fine-textured soils were not always lower. Soil properties such as soil structure might exert a more important influence in some circumstances. The selective erosion of clay particles was the main reason for N enrichment, as implied by the significant positive correlation between the ER of total nitrogen and clay fraction in eroded sediments. Significant regression equations between ERN and sediment yield were obtained for two pairs of soils, which were artificially categorized by soil texture. The one for fine-textured soils had greater intercept and more negative slope. Thus, the initially higher ERN would be lower than that for the other two soils with coarser texture once the sediment yield exceeded 629 kg ha?1. 相似文献
84.
Chen Yujun Guan Bin Wu Xingze Guo Jiangfeng Ma Zeren Zhang Jinhe Jiang Xing Bao Shibo Cao Yiyan Yin Chengdong Ai Di Chen Yuxuan Lin He Huang Zhen 《Environmental science and pollution research international》2023,30(5):11246-11271
Environmental Science and Pollution Research - In recent years, with global climate change, the utilization of carbon dioxide as a resource has become an important goal of human society to achieve... 相似文献
85.
甲酸、乙酸和草酸是降水中有机酸的主要成分。研究选用离子色谱法同时测定降水中的甲酸、乙酸和草酸,并对降水样品中3种有机酸的保存条件进行了研究。优化后的色谱条件为4. 0 mmol/L Na_2CO_3和1. 2 mmol/L NaHCO_3混合淋洗液,淋洗液流速为1. 0 m L/min,进样体积为200μL,电导池温度为30℃,柱温为室温。甲酸、乙酸和草酸的检出限分别为0. 002、0. 005、0. 005 mg/L,实际降水样品测定时平行样的相对标准偏差为1. 4%~12%,加标回收率为95%~118%。样品采集后需尽快用0. 45μm聚醚砜微孔滤膜过滤,4℃以下冷藏密封保存,2 d内测定。若用氢氧化钠溶液调节p H至8~10,样品可保存7 d。 相似文献
86.
为研究建筑废物红砖和工业废物煤渣用作人工湿地脱氮基质的可行性,分别通过静态吸附实验和动态NHf—N去除效果实验进行考察。结果表明,红砖和煤渣对NH4+-N最大静态吸附量分别为0.2533mg/g和0.0533mg/g,其吸附等温曲线均符合Freundlich型吸附方程,吸附常数分别为0.0419和0.0091;红砖煤渣组合对污水中NH4+-N平均动态脱除率达到41.18%,高于红砖的37.63%和煤渣的30.92%。 相似文献
88.
预测地层破裂压力是地下流体注入工程中的关键问题,关系到工程的稳定性和安全性。根据地测资料,岩石的抗拉强度会随着围压产生变化,然而目前常见的地层破裂压预测模型均未考虑该因素。基于厚壁圆筒法,针对2种砂岩开展不同围压条件下的砂岩致裂试验,根据试验数据,计算各组试验中试样的抗拉强度,并拟合围压与岩石抗拉强度的关系函数。研究岩石抗拉强度随围压变化的规律,提出能在实际地层中表征该规律的参数,基于该参数对现有的地层破裂压模型进行修正,并结合实测数据验证修正模型的可靠性。研究结果表明:岩石的抗拉强度随着围压的增加呈现明显的线性正相关关系,低围压下,新模型的预测结果与实测数据较为接近。随着围压增加,二者的差异逐渐增大,说明选取的特征参数在低围压下能较好地描述抗拉强度受围压的影响效应,而高围压下参数的取值需进一步研究。 相似文献
89.
盐度对模拟餐厨垃圾发酵液产聚羟基脂肪酸酯工艺的影响 总被引:1,自引:0,他引:1
利用餐厨垃圾发酵液生产聚羟基脂肪酸酯(PHA)可以在废物处理的同时实现有价资源回收。为探究发酵液中盐分对产PHA菌群富集过程的影响,以模拟餐厨垃圾发酵液为底物,研究了盐度存在下污泥理化性质、富集过程主要指标及菌群PHA合成能力等变化。结果表明,未经盐度富集的菌群易受到盐度抑制,在15 g·L~(-1)的盐度条件下,污泥PHA最大合成量可降至39.9%。富集过程中盐度的增加有利于污泥沉降性的提升,低盐度(5 g·L~(-1))下菌群分泌胞外聚合物量最多,达49.8 mg·g~(-1)(以VSS计),对菌群保护能力最强。不同盐度条件下的富集系统皆能保持较好的生态选择压力,但盐度对微生物生长的抑制随着浓度的增大而增强。经过盐度存在下长期富集后的污泥,在高盐度(10、15 g·L~(-1))底物条件下,仍能获得较高的PHA最大合成能力,但其较低的生长活性不利于最终PHA产量的提升,短期富集下,高盐度会抑制PHA的合成;而低盐度(5 g·L~(-1))有助于提高PHA合成能力,最高达50.5%。 相似文献
90.
Di Bernardino Annalisa Monti Paolo Leuzzi Giovanni Querzoli Giorgio 《Environmental Fluid Mechanics》2020,20(4):987-1005
Environmental Fluid Mechanics - We present results from water-channel experiments on neutrally-stable turbulent flows over staggered arrays of cubical obstacles modelling idealised urban canopies.... 相似文献