超高强度钻杆低温断裂性能及裂纹扩展特征研究

超高强度钻杆在冬季低温环境下容易发生脆性断裂事故,为了从断裂力学角度揭示其冷脆现象的本质,采用ZBC2302-D型示波冲击试验机,获得了不同温度下超高强度钢在冲击断裂过程中的力-位移曲线,并对比分析了冲击功、起裂功和裂纹扩展功之间的变化关系。采用国家标准GB 4161—2007中的计算公式,计算了冲击试样的裂纹扩展量Δa和阻抗应力强度因子K_R;同时,引入K_R阻力曲线,得到超高强度钻杆在不同温度下的剩余强度图。结果表明,当冲击试样开始出现裂纹时,随温度降低,钻杆的初始起裂应力有所增加,出现硬化现象。当钻杆出现一定长度的裂纹时,随温度降低,阻抗应力强度因子越来越小,而且降低速度越来越快,剩余强度也表现出相同的变化趋势。随温度降低,材料抵抗裂纹扩展的能力逐渐下降,表明钻杆在低温下更容易断裂。     

When and how to use Q methodology to understand perspectives in conservation research

Understanding human perspectives is critical in a range of conservation contexts, for example, in overcoming conflicts or developing projects that are acceptable to relevant stakeholders. The Q methodology is a unique semiquantitative technique used to explore human perspectives. It has been applied for decades in other disciplines and recently gained traction in conservation. This paper helps researchers assess when Q is useful for a given conservation question and what its use involves. To do so, we explained the steps necessary to conduct a Q study, from the research design to the interpretation of results. We provided recommendations to minimize biases in conducting a Q study, which can affect mostly when designing the study and collecting the data. We conducted a structured literature review of 52 studies to examine in what empirical conservation contexts Q has been used. Most studies were subnational or national cases, but some also address multinational or global questions. We found that Q has been applied to 4 broad types of conservation goals: addressing conflict, devising management alternatives, understanding policy acceptability, and critically reflecting on the values that implicitly influence research and practice. Through these applications, researchers found hidden views, understood opinions in depth and discovered points of consensus that facilitated unlocking difficult disagreements. The Q methodology has a clear procedure but is also flexible, allowing researchers explore long‐term views, or views about items other than statements, such as landscape images. We also found some inconsistencies in applying and, mainly, in reporting Q studies, whereby it was not possible to fully understand how the research was conducted or why some atypical research decisions had been taken in some studies. Accordingly, we suggest a reporting checklist.     

Estimating abundance without recaptures of marked pallid sturgeon in the Mississippi River

Abundance estimates are essential for assessing the viability of populations and the risks posed by alternative management actions. An effort to estimate abundance via a repeated mark‐recapture experiment may fail to recapture marked individuals. We devised a method for obtaining lower bounds on abundance in the absence of recaptures for both panmictic and spatially structured populations. The method assumes few enough recaptures were expected to be missed by random chance. The upper Bayesian credible limit on expected recaptures allows probabilistic statements about the minimum number of individuals present in the population. We applied this method to data from a 12‐year survey of pallid sturgeon (Scaphirhynchus albus) in the lower and middle Mississippi River (U.S.A.). None of the 241 individuals marked was recaptured in the survey. After accounting for survival and movement, our model‐averaged estimate of the total abundance of pallid sturgeon ≥3 years old in the study area had a 1%, 5%, or 25% chance of being <4,600, 7,000, or 15,000, respectively. When we assumed fish were distributed in proportion to survey catch per unit effort, the farthest downstream reach in the survey hosted at least 4.5–15 fish per river kilometer (rkm), whereas the remainder of the reaches in the lower and middle Mississippi River hosted at least 2.6–8.5 fish/rkm for all model variations examined. The lower Mississippi River had an average density of pallid sturgeon ≥3 years old of at least 3.0–9.8 fish/rkm. The choice of Bayesian prior was the largest source of uncertainty we considered but did not alter the order of magnitude of lower bounds. Nil‐recapture estimates of abundance are highly uncertain and require careful communication but can deliver insights from experiments that might otherwise be considered a failure.     

受限空间内惰性气体对CH4爆炸抑制特性研究

N2和CO2是常用的惰性抑爆气体,为研究两种气体的抑爆特性,采用20L球形爆炸试验装置,分析了不同浓度配比条件下N2/CH4/空气以及CO2/CH4/空气混合气体的爆炸压力,同时采集爆炸后的气体样品,对比分析爆炸后残留气体的主要成分。结果显示:随CH4浓度从5%增加至12.5%时,完全抑制CH4爆炸需要的惰性气体最小量先增大后降低,CH4浓度在6.5%~7.5%之间时,抑爆需要的惰性气体的量最大;在同一CH4浓度条件下,抑爆需要N2的量大于CO2,并且CH4浓度在5%~6.5%时,抑爆需要两种惰性气体的量值差别最大;当CH4浓度一定时,随着加入惰性气体量的增大,爆炸最大超压逐渐降低,惰性气体浓度和爆炸超压之间基本呈线性关系;在同样条件下,相对于N2,CO2为抑爆气体时,爆炸后腔体内残留的CH4浓度较高。研究成果为惰性气体抑爆技术提供技术支撑,同时为揭示惰性气体抑爆机理有一定作用。     

PLC控制系统在钢渣热焖工艺中的应用

利用PLC控制系统,实现在钢渣热焖工艺中的恒压供水和钢渣热焖定时定量喷水的自动控制要求,具有国际先进水平,取得了良好的经济效益、社会效益和环境效益.     

船用E500钢在海水中阴极极化氢脆敏感性研究

目的研究阴极保护电位对E500钢在海水中氢脆敏感性的影响。方法采用慢应变速率拉伸试验(SSRT),同时利用三电极体系进行不同电位极化,并结合扫描电镜进行试样断口观察。结果随着阴极保护电位负移,E500钢在海水中的氢脆敏感性增加,阴极保护电位为-0.95 V(vs.SCE)时,拉伸试样出现脆性解理断裂特征,电位为-1.00 V时,E500钢断口呈脆性断裂特征。结论根据氢脆系数拟合曲线得出,当氢脆系数达到25%时,E500钢最负阴极保护电位应为-0.913 V。     

热带海洋大气环境下X70管线钢的缝隙腐蚀行为研究

目的研究X70管线钢在热带海洋大气实海环境下的缝隙腐蚀行为。方法在距离湛江东海岛海岸50m和200 m处分别搭建楔型缝隙模型,安装大气环境Cl-收集装置和自动气象监测站。结果距离海岸越近,风速越大,大气中Cl-沉降速率也越大,X70管线钢缝隙腐蚀越严重。X70管线钢在距离海岸50 m处发生缝隙腐蚀的最大缝宽约为0.96 mm,200 m处最大缝宽约为3.75 mm,50 m处缝隙腐蚀更严重。结论缝隙腐蚀区域形成了氧浓差电池,同时随着缝隙液中Cl-向缝隙内迁移,发生闭塞区电池自催化过程,在二者共同作用下,缝隙腐蚀区域较非缝隙腐蚀区域腐蚀更严重。     

外加微量N2H4下SBR中硝化微生物特性

运行实验室规模单级硝化序批式反应器(SBR),研究长期外加微量N_2H_4(约3 mg·L~(-1))对硝化污泥中功能微生物好氧氨氧化菌(AOB)、亚硝酸盐氧化菌(NOB)的影响.结果表明,外加微量N_2H_4的硝化污泥中,AOB主要属于亚硝化球菌(Nitrosococcu)属和亚硝化单胞菌(Nitrosomonas)属,另有少部分属于亚硝化螺旋菌(Nitrosospira)属,NOB属于硝化杆菌(Nitrobacter)属.外加微量N_2H_4前后,AOB amoA基因拷贝数(以干污泥计)由1.0×10~9copies·g~(-1)减少为2.09×10~4copies·g~(-1),NOB nxrB基因拷贝数由1.28×10~7copies·g~(-1)减少为2.56×10~5copies·g~(-1).AOB对环境因素较NOB相比更为敏感,N_2H_4对硝化微生物的抑制与毒性作用使外加微量N_2H_4的硝化污泥中AOB流失幅度大于NOB,但定量PCR方法无法准确比较N_2H_4对AOB与NOB活性抑制的强弱.长期外加微量N_2H_4破坏硝化微生物活性,使反应器崩溃.因此在没有厌氧氨氧化菌(AnAOB)消耗N_2H_4的亚硝化系统中,企图通过调控外加N_2H_4浓度水平抑制NOB活性,从而进一步洗脱NOB提高脱氮性能可能无法实现.     

添加不同 N源条件下典型除草剂对土壤呼吸和 N2O排放的影响

通过室内土壤培养实验,采用间歇密闭培养-气相色谱法研究了添加不同N源条件下我国典型旱地除草剂对农田土壤呼吸和N2O排放的影响.结果表明,在添加（NH4）2SO4氮源条件下,莠去津和百草枯对土壤呼吸和N2O排放无显著影响（P〉0.05）.草甘膦显著抑制了土壤呼吸（P〈0.05）,是对照的78.5%,N2O的排放无显著影响（P〉0.05）,仅表现为均值降低了20.1%.苯磺隆显著促进了土壤呼吸（P〈0.05）,是对照的1.1倍,对N2O排放也无显著影响（P〉0.05）.乙草胺显著促进了土壤呼吸和N2O的排放（P〈0.05）,分别是对照的1.1和1.5倍.在添加尿素的条件下,莠去津和乙草胺对土壤呼吸和N2O排放无显著影响（P〉0.05）.百草枯显著促进了N2O的排放（P〈0.05）,是对照的1.4倍,却对土壤呼吸无显著影响（P〉0.05）.草甘膦显著抑制了土壤呼吸（P〈0.05）,仅为对照的82.5%,对N2O的排放却无显著影响（P〉0.05）.苯磺隆显著促进了土壤呼吸和N2O的排放（P〈0.05）,其分别是对照的1.3和1.6倍.鉴于不同除草剂对不同微生物生理代谢影响的复杂性,其对温室气体的作用和影响还需长期田间试验研究.