冷拔无缝钢管爆裂分析

在无缝钢管的冷拔过程中,存在着冷作硬化和氢脆现象,它们是造成钢管爆裂的主要原因。此文对两个现象进行了分析,提出了一些防止钢管爆裂的措施。     

过氧化氢加Fe~(3+)作催化剂处理含酚废水的研究

采用H_2O_2/Fe~(3+)对合酚废水进行了催化氧化的研究。对于溶液pH值、过氧化氢浓度、铁离子浓度与酚、COD、TOC去除的关系作了探讨。结果表明,在酸性pH值范围内,Fe~(3+)作催化剂可获得不低于Fe~(2+)作催化剂时的催化活性,对酚、COD和TOC都有较好的去除率。而在初始pH=7时,Fe~(3+)作催化剂的反应活性明显降低。自动连续控制溶液pH=7.0±0.2时,无论是高铁或低铁离子都大幅度降低其反应活性。同时也证实,低浓度铁离子不论是Fe~(3+)或Fe~(2+)也都降低其催化反应活性。     

重庆开县井喷事故的环境影响分析

重庆开县“12.23”井喷事故中,大量富含硫化氢的天然气排入周围环境,致使以高桥镇为核心区的4个乡镇28个村,受到不同程度的硫化氢污染。笔者根据污染物排放情况以及当地的气候、水文等条件分析了井喷事故对该地区大气环境、水环境和土壤环境所造成的影响。结果表明,在距离井喷事故污染源下风方向5000m以内的区域,以及在与下风方向相垂直的方向500m以内的区域,大气环境均受到了不同程度的硫化氢污染,且在500～1500m区域内,污染最为严重。同时,由于硫化氢的沉降,该地区的水和土壤环境也受到了不同程度的影响。     

定氢仪在环境试验中的应用

本文叙述了定氢仪的测氢原理、结构、特点及定氢仪在环境试验中的用途。     

固定污染源非甲烷总烃自动连续监测系统比对监测

对非甲烷总烃自动连续监测系统进行示值误差、响应时间、零点漂移和量程漂移等性能测试,对非甲烷总烃便携式分析仪进行检出限、精密度、准确度等性能测试。性能测试满足相关要求后同时利用便携式催化氧化-氢火焰离子化检测器法(催化氧化-FID)、便携式气相色谱-氢火焰离子化检测器法(GC-FID)和实验室气相色谱-氢火焰离子化检测器法(GC-FID)对固定污染源非甲烷总烃自动连续监测系统进行现场比对测试。测试结果表明,在工况变动较大的情况下,便携式FID法与实验室GC-FID法测试结果相对误差为19. 6%～35. 1%,具有很好的可比性。以实验室GC-FID法为参比方法时,自动连续监测系统相对准确度为64. 1%,不满足《固定污染源废气非甲烷总烃连续监测系统技术要求及检测方法》(HJ 1013—2018)的要求。以便携式FID为参比方法时,自动连续监测系统相对准确度分别为28. 6%和35. 3%,相对《固定污染源废气总烃、甲烷和非甲烷总烃的测定气相色谱法》(HJ 38—2017)方法一致性更好,均能满足《HJ 1013—2018》的要求。提出,应推进便携式方法在自动连续监测系统验收和质控比对中的应用。     

处理焦化废水中难生物降解的有机毒物的研究

研究了Fenton试剂(H₂O₂+Fe2+)在紫外光(UV)幅照下,氧化处理焦化废水中难被生物降解的有机毒物的可行性,并对反应条件进行了优化,结果表明此法对焦化废水中包括多环芳烃(PAH)的所有有机毒物都有较强的去除能力。但如何降低处理费用,有待进一步工作。      

The role of a changing Arctic Ocean and climate for the biogeochemical cycling of dimethyl sulphide and carbon monoxide

Dimethyl sulphide (DMS) and carbon monoxide (CO) are climate-relevant trace gases that play key roles in the radiative budget of the Arctic atmosphere. Under global warming, Arctic sea ice retreats at an unprecedented rate, altering light penetration and biological communities, and potentially affect DMS and CO cycling in the Arctic Ocean. This could have socio-economic implications in and beyond the Arctic region. However, little is known about CO production pathways and emissions in this region and the future development of DMS and CO cycling. Here we summarize the current understanding and assess potential future changes of DMS and CO cycling in relation to changes in sea ice coverage, light penetration, bacterial and microalgal communities, pH and physical properties. We suggest that production of DMS and CO might increase with ice melting, increasing light availability and shifting phytoplankton community. Among others, policy measures should facilitate large-scale process studies, coordinated long term observations and modelling efforts to improve our current understanding of the cycling and emissions of DMS and CO in the Arctic Ocean and of global consequences.     

分光光度法与离子色谱法测定空气中氯化氢的对比研究

通过对硫氰酸汞分光光度法和离子色谱法测定空气中氯化氢含量的对比发现,两种方法对实验室质控样和实际样品的分析测定均能达到要求,且F检验法分析表明实测结果没有显著性差异。然而,硫氰酸汞分光光度法的测试过程操作繁琐,误差较大,稳定时间较长,且硫氰酸汞具有剧毒,危害操作人员的健康,残液也难以处理。离子色谱法分析操作简单,过程安全可靠,能够有效降低样品受污染的可能性并保证分析质量。     

Unexpected difference in phenol sorption on PTMA- and BTMA-bentonite

The comparison of phenol sorption on phenyltrimethylammonium (PTMA)- and benzyltrimethylammonium (BTMA)-bentonite shows a clear difference as far as phenol sorption isotherms are concerned. For PTMA-bentonite the sorption isotherm is of a straight-line character which results from simple partitioning of phenol between the aqueous and organic phases sorbed on the bentonite surface. For BTMA-bentonite the isotherm has a convex shape, characteristic of physicochemical sorption.For the first time a three-parametric model, including the dissociation constant of phenol pK_a, distribution constant of phenol Kd_phen and phenolate anion Kd_phen⁻ between the aqueous phase and the bentonite phases is used for the evaluation of phenol sorption on organoclays with pH change. The model shows that the values of Kd_phen are higher than those of Kd_phen⁻ for all investigated initial phenol concentrations.The inspection of the FTIR spectrum of BTMA-bentonite loaded with phenol in the regions 1300–1600 and 1620–1680 cm⁻¹ shows the features of π–π electron interaction between the benzene rings of phenol and the BTMA cation together with the phenol–water hydrogen bond strengthened by this interaction.     

Detailed and reduced chemistry for hydrogen autoignition

Reaction-rate parameters are given for the detailed chemistry of gas-phase hydrogen combustion, involving 21 reversible elementary steps. It is indicated that, when attention is restricted to specific combustion processes and particular conditions of interest, fewer elementary steps are needed. In particular, for calculating autoignition times over a wide range of pressures for temperatures between about 1000 and 2000 K, five irreversible elementary steps suffice, yielding a remarkable reduction in complexity. It is explained that, from a mathematical viewpoint, in terms of global reaction-kinetic mechanisms, the hydrogen–oxygen system in principle comprises only six overall steps. Rational reduced chemical mechanisms for hydrogen combustion therefore necessarily must have fewer than six overall steps. For autoignition over the range of conditions specified above, ignition times can be determined accurately by considering, in addition to an elementary initiation step and an elementary termination step, at most three overall steps for reaction intermediaries, which reduce to two for very fuel-lean conditions and to one for stoichiometric or fuel-rich conditions. The resulting reductions can simplify computations that need to be performed in risk analyses for hydrogen storage and utilization.