Bi2MoO6/纳米棒ZnO异质结对MB的可见光-压电协同降解性能研究

采用水热法合成了一系列不同负载率的Bi₂MoO₆/纳米棒ZnO复合光催化剂.通过XRD、FT-IR、SEM、TEM、XPS、UV-Vis、EPR和PL等分析技术对合成的样品进行表征.在光/超声波条件下,以亚甲基蓝（MB）为目标降解物评价其压电-光催化性能.结果表明：Bi₂MoO₆/ZnO纳米棒（BZ-0.6）的降解速率常数约为ZnO传统光催化的9.25倍,其性能提升的主要原因在于ZnO的压电效应与Bi₂MoO₆/ZnO界面形成的异质结的耦合,有效地促进了电子和空穴的分离和转移.此外,同实验条件下,循环利用5次后Bi₂MoO₆/ZnO复合光催化剂降解率仍保持良好的稳定性.     

长三角区域一体化高质量发展：问题与出路

长三角一体化高质量发展对于中国经济行稳致远有着不言而喻的重要意义。为了科学全面认识新时代长三角一体化高质量发展中存在的问题,厘清未来的发展出路,邀请来自不同领域的相关专家就长三角一体化高质量发展中的区域协调、产业协同、交通组织、城镇体系演变、跨区合作、要素配置、流域统筹、一体化路径、绿色低碳发展等研究前沿进行访谈。访谈结果表明：长三角作为我国经济发展最活跃、开放程度最高、创新能力最强的区域,其发展中仍然存在内部发展不平衡、区间交通割裂、行政壁垒尚存、流域生态协作不健全、产业协同发展不足、绿色经济体系较弱等突出问题。长三角在中国乃至世界发展格局中的战略地位,需要综合各学科各专业的理论知识,从不同视角持续关注长三角一体化高质量发展的重大科学命题。紧扣“一体化”和“高质量”,长三角一体化首先要创新机制缩小区域内部发展差异,强化综合交通一体化的基础支撑,更要突破行政边界的制约;其次要创新机制体制来保障生产要素的有效流动与配置,通过价值链、产业链、创新链的融合发展来夯实一体化;再次要促进土地要素向长三角集中使用,提高长三角地区土地承载能力,为长三角区域一体化高质量发展提供充足的土地要素保证;然后要优化人口就业空间结构,加强城际间环境污染联防联治,强化大江大河等重大流域的省际统筹与合作,共同提升长三角的生态系统服务功能,推动绿色一体化发展;最后更要贯彻五大新发展理念,通过科研突破与市场机制来实现低碳发展,在创新驱动引领下打造流空间世界级枢纽,以实现长三角区域一体化高质量发展的新局面。以上观点为长三角区域一体化高质量发展提供科学可行的理论和决策支持。     

铁基硅盐对土壤环境镉砷赋存形态及转化影响

为探明铁基硅盐对土壤镉砷赋存形态影响及各形态间转化规律,采用室内长期淹水培养吸附实验,研究不同比例铁硅材料对土壤离子态镉砷活性影响;筛选适宜铁基硅盐(FS)配比同时添加腐殖酸(FSC)和金属氧化物(FSCa),明确复配处理土壤中镉砷分级形态转化程度.结果显示,铁:硅比值增加10%,土壤pH值平均降低0.35;F₂-S₈处理土壤离子态镉降幅71%;F₁₀-S₀处理土壤离子态砷降低59.9%,离子态镉砷含量与硅酸盐-铁盐施用量互呈反比;处理F₄-S₆和F₆-S₄之间镉、砷钝化率产生交点,约为25%~30%.土壤中镉主要以可溶态为主,占比58%;砷主要以铁铝氧化态和钙结合态为主,占比40%和23%.铁硅比例为5:5或5.5:4.5左右复配能有效将铝结合态砷和铁铝氧化态砷转变为钙结合态砷和残渣态砷,可溶态镉转化为碳酸盐结合态镉以及铁锰氧化态镉,同步降低土壤中镉砷的活性.     

污泥基生物炭结构的共焦显微拉曼技术应用

采用共焦显微拉曼光谱仪探索不同热解温度(500~900)℃条件下所制备的污泥基生物炭结构变化的表征方法.结果表明,拉曼信号的荧光干扰与生物炭的理化特性有较强的相关性.随着热解温度升高,拉曼漂移系数减小,这与污泥基生物炭挥发分含量、H/C和O/C比变化趋势一致.其中,漂移系数与挥发分含量和H/C的相关性指数分别是0.97和0.94,其变化规律可用来准确评估生物炭挥发分含量和H/C的变化.同时,生物炭在拉曼光谱中的特征峰强度比D/G随着热解温度升高而增强,代表了污泥基生物炭无序化程度增加的过程.谷区域(V)与D峰强度比IV/ID随热解温度升高而减小,表明具有缺陷的稠合芳环结构的比例增加;另外,经分峰拟合后得到的ID1/IG1变化较小,而ID2/IG2呈增加趋势,证实了小分子侧链基团断裂形成的化合物部分沉积在炭表面,形成缺陷和非晶结构;IG1/IG2随着热解温度升高而减小,表明了炭基材料键角有序与无序比随着热解温度的升高而降低.因此,拉曼光谱可用于表征污泥基生物炭的微观结构变化,反映其结构演变规律.     

2018年山东近岸养殖区营养盐结构及限制特征

本研究依据2018年山东近岸养殖区调查资料,采用营养盐限制法则评价方法,对DIN、PO₄-P、SiO₃-Si的平面分布、结构及限制特征进行了分析。结果显示,2018年,山东近岸养殖区DIN、PO₄-P和SiO₃-Si年平均浓度分别为（0.253±0.048）mg/L、（0.00743±0.00238）mg/L和（0.269±0.089）mg/L,渤海养殖区片的DIN、SiO₃-Si浓度总体高于黄海养殖区片,高值站位多分布于莱州湾等半封闭海湾;PO₄-P浓度均普遍较低。N/P、Si/N和Si/P的年平均值分别为131±47、0.92±0.47和90±60。N/P高值区多分布于渤海养殖区及海阳－莱阳区片;Si/N、Si/P高值区多分布于牟平区片及渤海的潍坊、龙口及莱州－招远区片。对营养盐限制状况的分析表明,山东近岸养殖区营养盐结构表现为明显的磷限制和枯水期的硅限制。4个季节磷限制状况都较为明显,枯水季节的冬季、春季和秋季硅限制较为明显。建议滩涂贝类养殖区片合理规划放养密度,充分利用海洋初级生产力,净化水质;筏式养殖贝类、藻类养殖区片积极推广贝藻兼养、轮养,开展时空立体养殖,调整养殖品种结构,改善因营养结构改变导致的贫营养状况。     

凌水湾不同海岸结构潮间带附着生物群落特征差异性影响分析

研究不同海岸结构潮间带生物群落特征的差异不仅可以了解结构的基质特征与潮间带生物栖息适宜度的关系,还可为人工岸线生态化措施的选择提供依据。本文对凌水湾自然岸线和6个不同海岸结构潮间带生物群落进行了调查,比较了潮间带生物群落特征在不同海岸结构之间的差异,探讨了基质和结构特征与潮间带附着生物指标的关系,总结了影响附着生物特征...     

Co-metabolic transformation of the neonicotinoid insecticide imidacloprid by the new soil isolate Pseudoxanthomonas indica CGMCC 6648

A new imidacloprid (IMI) degrading bacterium Z-9 (deposited number CGMCC 6648) was isolated and identified as Pseudoxanthomonas indica by 16S rRNA gene analysis. Two metabolites were identified as olefin and 5-hydroxy IMI by liquid chromatography-mass spectrometry and nuclear magnetic resonance analysis. P. indica CGMCC 6648 degraded 70.1% of IMI (1.22 mmol L^?1) and formed 0.93 mmol L^?1 5-hydroxy IMI and 0.05 mmol L^?1 olefin IMI in 6 days and in the presence of 100 mmol L^?1 glucose. The half-life of IMI degradation was 3.6 days. P. indica CGMCC 6648 transforms IMI via a co-metabolism mechanism and different carbohydrates have significant effects on 5-hydroxy IMI formation, whereas different organic acids have substantial effects on olefin IMI production. Lactose is the best co-substrate for IMI degradation and 5-hydroxy IMI formation with 0.77 mmol L^?1 degraded and 0.67 mmol L^?1 formed in 48 h, respectively. Pyruvate is the best co-substrate for olefin IMI formation with 0.17 mmol L^?1 produced in 96 h for all carbon sources tested. Pyruvate significantly stimulates the conversion of 5-hydroxy IMI to olefin IMI, whereas glucose slightly inhibits this reaction. P. indica CGMCC 6648 rapidly degrades IMI and forms olefin IMI, which may enhance its potential for biodegradation of IMI and increase its insecticidal activity, which can decrease the IMI dosage required.     

Differences in nitrous oxide fluxes from red soil under different land uses in mid-subtropical China

Red soil may play an important role in nitrous oxide (N₂O) emissions due to its recent land use change pattern. To predict the land use change effect on N₂O emissions, we examined the relationship between soil N₂O flux and environmental determinants in four different types of land uses in subtropical red soil. During two years of study (January 2005-January 2007), biweekly N₂O fluxes were measured from 09:00 to 11:00 a.m. using static closed chamber method. Objectives were to estimate the seasonal and annual N₂O flux differences from land use change and, reveal the controlling factors of soil N₂O emission by studying the relationship of dissolved organic carbon (DOC), microbial biomass carbon (MBC), water filled pore space (WFPS) and soil temperature with soil N₂O flux. Nitrous oxide fluxes were significantly higher in hot-humid season than in the cool-dry season. Significant differences in soil N₂O fluxes were observed among four land uses; 2.9, 1.9 and 1.7 times increased N₂O emissions were observed after conventional land use conversion from woodland to paddy, orchard and upland, respectively. The mean annual budgets of N₂O emission were 0.71-2.21 kg N₂O-N ha⁻¹ year⁻¹ from four land use types. The differences were partly attributed to increased fertilizer use in agriculture land uses. In all land uses, N₂O fluxes were positively related to soil temperature and DOC accounting for 22-48% and 30-46% of the seasonal N₂O flux variability, respectively. Nitrous oxide fluxes did significantly correlate with WFPS in orchard and upland only. Nitrous oxide fluxes responded positively to MBC in all land use types except orchard which had the lowest WFPS. We conclude that (1) land use conversion from woodland to agriculture land uses leads to increased soil N₂O fluxes, partly due increased fertilizer use, and (2) irrespective of land use, soil N₂O fluxes are under environmental controls, the main variables being soil temperature and DOC, both of which control the supply of nitrification and denitrification substrates.     

Fatty acids and algal lipids as precursors of chlorination by-products

Six common algal fatty acids (FAs) with different numbers of double bonds, lipophilic fractions and proteins extracted from the diatom Navicula pelliculosa and algal cells were chlorinated to evaluate their potential in generating disinfection by-products (DBPs). The result showed that the more double bonds in the FAs, the higher the amounts of chloroform and dichloroacetic acid (DCAA) produced, but such a pattern was not observed for trichloroacetic acid (TCAA). Based on the previously reported composition of fatty acids in algal lipids, the DBP generation potentials of algal lipids were calculated. These predicted values were much lower than those measured in the chlorinated algal lipophilic fraction, suggesting unknown lipophilic fraction(s) served as potent DBPs precursors. Another calculation attempted to predict DBP production in algal cells based on algal lipid and protein composition, given quantified measured DBP production per unit algal lipid and proteins. The analysis showed that the observed DBP production was similar to that predicted (< 35% difference), suggesting that algal biochemical compositions may serve as a bioindicator for preliminary estimation of chloroform, DCAA and TCAA formation upon chlorinating algae.