油品火灾扬沸前兆现象的实验研究

本文研究典型油品扬沸前兆期的火行为。应用火焰显示技术观察扬沸前兆期的火焰结构；测量扬沸过程中油、水层的温度——时间历程；在时域、频域上分析扬沸前兆的微爆噪声特性；并在原理上提出诊断，预报油品火灾扬沸发生的新途径。     

Soil carbon pool in China and its global significance

ＳｏｉｌｃａｒｂｏｎｐｏｏｌｉｎＣｈｉｎａａｎｄｉｔｓｇｌｏｂａｌｓｉｇｎｉｆｉｃａｎｃｅ￥ＦａｎｇＪｉｎｇｙｕｎ，ＬｉｕＧｕｏｈｕａ，ＸｕＳｏｎｇｌｉｎｇ（ＲｅｓｅａｒｃｈＣｅｎｔｅｒｆｏｒＥｃｏ－ＥｎｖｉｒｏｎｍｅｎｔａｌＳｃｉｅｎｃｅ，Ｃｈｉｎ...     

呼伦贝尔草原土壤粘粉粒组分对有机碳和全氮含量的影响

土壤在维持全球碳、氮循环中起着重要的作用。利用土壤粒级分组的方法,分析了呼伦贝尔草原土壤有机碳、全氮、阳离子交换量,并探讨其空间差异与成因。结果表明,(1)在呼伦贝尔草原,土壤有机碳(SOC)、全氮(TN)在不同地质发育的土壤类型中变异较大,而土壤粘粉粒组分中的有机碳(SOCclay-silt)、全氮(TNclay-silt)质量分数变异较小。在土壤表层(0~20cm),SOC、TN质量分数分别介于0.24%~3.70%、0.0316~0.3403mg/kg,而SOCclay-silt、TNclay-silt平均质量分数分别为3.61%±0.50%、0.3440%±0.0251%。在土壤下层(20~40cm),SOC、TN质量分数分别介于0.13%~2.91%、0.0175~0.2511mg/kg,而SOCclay-silt、TNclay-silt平均值分别为2.65%±0.63%、0.2622%±0.0923%。(2)土壤有机碳、全氮与土壤粘粉粒比例之间呈显著的正相关,表明土壤粘粉粒比例愈高,土壤有机碳和全氮在土壤中稳定性就愈强。     

北京动物园水禽湖溶解氧动态与喷泉增氧效果分析

对北京动物园水禽湖的溶解氧动态规律进行了分析研究 ,根据得出的结果及动物园特殊的环境特征 ,提出了采用喷泉增氧的方式来改善水禽湖的溶解氧状况 ,同时对喷泉的增氧效果作了分析     

合建式完全混合曝气池处理能力评价及改造初探

根据生物曝气池几年来的运行实践，对其主要设计参数进行复核，为了达到设计处理能力，对生化曝气池的改造提出个人的看法并做初步探讨     

浮式LNG平台串靠卸载泄漏后果影响分析

浮式LNG生产储卸装置(FLNG)作为新兴的深海气田生产装置,集天然气生产、液化、储存和装卸功能于一身,其卸载方式主要有旁靠卸载和串靠卸载2种,其中串靠卸载因能适应恶劣海况而备受深海作业欢迎,但串靠卸载的泄漏后果和影响尚不明确,因此研究恶劣海况下LNG串靠卸载的泄漏风险及后果尤为迫切和重要。考虑海上极端气象条件,采用DNV公司的PHAST软件,定量计算FLNG串靠卸载方式在卸载臂发生小孔、中孔、大孔泄漏及全尺寸破裂时,LNG泄漏后产生的具有火灾爆炸危险性的蒸汽隔离区域,根据伤害阈值明确LNG导致人员低温冻伤和窒息的最小距离,并对可能发生的喷射火、池火和蒸汽云爆炸等恶劣事故造成的后果进行预测。     

氮添加对亚热带森林土壤有机碳氮组分的影响

为了研究氮添加对森林土壤有机碳氮组分稳定性的影响,选取我国亚热带典型常绿阔叶林(浙江桂天然林和罗浮栲天然林)和针叶林(杉木人工林),开展为期5年的野外模拟氮沉降试验,分别设置对照〔0 kg/(hm2·a),以NH₄NO₃中的N计,下同〕、低氮〔75 kg/(hm2·a)〕和高氮〔150 kg/(hm2·a)〕3个氮添加水平,用H₂SO₄分2步酸水解获得LPⅠ(活性有机库Ⅰ)、LPⅡ(活性有机库Ⅱ)和RP(惰性有机库),定量研究土壤活性和惰性有机碳氮组分以及微生物生物量碳氮对氮添加的响应. 结果表明:氮添加仅对w(LPⅡ-C)(LPⅡ-C为活性有机碳Ⅱ)有显著影响,而对其他活性和惰性有机碳氮组分的影响不显著,并且对不同林分的影响存在差异. 与对照处理相比,低氮处理下浙江桂天然林、罗浮栲天然林和杉木人工林土壤w(LPⅡ-C)的增幅分别为15.3%、29.8%、68.8%;高氮处理下杉木人工林土壤w(LPⅠ-C)(LPⅠ-C为活性有机碳Ⅰ)、w(LPⅠ-N)(LPⅠ-N为活性有机氮Ⅰ)和w(RP-C)(RP-C为惰性有机碳)的增幅分别为32.4%、78.6%、28.7%;氮添加使得土壤w(SMB-C)(土壤微生物生物量碳)的增幅为18.1%~202.5%、w(SMB-N)(土壤微生物生物量氮)的增幅为0%~103.6%;在氮添加处理下,除杉木人工林土壤SMB-N/LPⅠ-N〔w(SMB-N)/w(LPⅠ-N)〕是随着氮添加水平的增加而降低外,微生物对其他林分土壤活性有机氮的利用均表现为随着氮添加水平的增加而增加. 研究显示,氮添加对阔叶林和针叶林土壤活性和惰性有机碳氮组分的影响存在差异,但差异不显著,这与它们归还土壤的凋落物性质差异有关,并且凋落物的分解差异也可能是影响土壤不同碳氮组分变化的原因.      

我国典型陆地生态系统固碳重要区范围界定

全球变暖已成为当今最主要的全球性环境问题之一,建立固碳重要区也是应对全球气候变化的重要途径之一.根据我国陆地生态系统现状以及固碳相关的最新研究结果和政府文件,以森林、草地生态系统为主要研究对象,采用GIS空间叠置分析方法,界定我国典型陆地生态系统固碳重要区(注:涉及“全国”的各要素范围均未包含港澳台地区)的空间范围.研究结果:固碳重要区评价指标体系包括生态系统碳储量、碳汇和固碳潜力3个核心因子,界定过程包括界定范围选择、固碳高值区识别、固碳重要区范围确定和分区命名等步骤.在全国尺度界定了森林、草地两大类共计20个固碳重要区,总面积285.6×104 km2.其中,森林生态系统固碳重要区主要分布在我国东北部、西南部的深山区和东南部的山地丘陵,草地生态系统固碳重要区主要分布在内蒙古高原中东部、新疆西北部山地和青藏高原东南部.固碳重要区面积占全国国土总面积的29.8%,所提供的NPP(净初级生产力)量占全国NPP总量的40.7%,固碳能力是全国平均水平的1.37倍.固碳重要区范围界定结果符合“以较小面积获取较大服务”原则,适于作为我国实现碳减排目标的优先保护区域.      

Experimental study of the evaporation of spreading liquid nitrogen

The investigation of cryogenic liquid pool spreading is an essential procedure to assess the hazard of cryogenic liquid usage. There is a wide range of models used to describe the spreading of a cryogenic liquid pool. Many of these models require the evaporation velocity, which has to be determined experimentally because the heat transfer process between the liquid pool and the surroundings is too complicated to be modeled. In this experimental study, to measure the evaporation velocity when the pool is spreading, liquid nitrogen was continuously released onto unconfined concrete ground. Almost all of the reported results are based on a non-spreading pool in which cryogenic liquid is instantaneously poured onto bounded ground for a very short period of time. For the precise measurement of pool spreading and evaporation weight with time, a cone-type funnel was designed to achieve a nearly constant liquid nitrogen release rate during discharge. Specifically, three nozzles with nominal flow rates of 3.4 × 10⁻² kg/s, 5.6 × 10⁻² kg/s and 9.0 × 10⁻² kg/s were used to investigate the effect of the release rate on the evaporation velocity. It is noted that information about the release rate is not necessary to measure the evaporation velocity in case of the non-spreading pool. A simultaneous measurement of the pool location using thermocouples and of the pool mass using a digital balance was carried out to measure the evaporation velocity and the pool radius. A greater release flow rate was found to result in a greater average evaporation velocity, and the evaporation velocity decreased with the spreading time and the pool radius.     

Effect of treated swimming pool water on the levels of trihalomethanes in swimmer's urine

Swimming pools are considered to be the prime source for public exposure to trihalomethanes (THMs), mainly chloroform, because of their use for hygienic purposes. High doses of chlorine are easily perceptible by smell. The aim of this study was to measure simultaneously the THM levels in urine and blood of swimmers and in pool water itself (from city and university swimming pool), in order to investigate further the relationship between substances in different matrices at known environmental levels with uptake of these substances in indoor swimming pools. Volatile analytes were isolated and preconcentrated from the samples by thin layer headspace analysis (TLHS) with autogenous generation of the liquid sorbent. Chloroform, bromodichloromethane and dibromochloromethane were detected in the urine of all persons attending a swimming pool. Concentrations of THM compounds varied in the case of each swimmer. The research confirmed that approximately 10% of the volatile haloorganic compounds are excreted in urine in the unchanged form.