钻井废水可生化性研究及处理技术探索

钻井废水是油气井开采钻探过程中产生的废水，钻井废水成分复杂，有机物浓度高、色度高、悬浮物浓度高，水质变化大，排放点分散，不经处理排放会污染环境，破坏生态。随着石油工业的不断发展和国家环保法律法规的日益严格，钻井废水的治理也越来越受到重视。如何采用经济有效的方法处理废弃钻井液，对油气井开采业的可持续发展具有重要意义。本论文以遂宁磨153 井的钻井废水为主要研究对象，在对废水进行絮凝沉降预处理和生物法处理探索的基础上，针对钻井废水可生化性差的特点，采用水解酸化和Fenton 试剂改善钻井废水的可生化性，对反应过程进行了比较详细的考察，对可生化性改善的机理进行了探索。主要研究结论如下：1 用PFS 和PAC 配制的混合混凝剂对钻井废水COD 的去除效果比较显著，在最佳条件下COD 的去除率可达75%，且絮体沉降速度较快，出水pH 保持中性；2 水解酸化法处理钻井废水可显著改善废水的可生化性。经48 小时水解酸化处理，钻井废水的理论BOD5可提高约22 倍，表观BOD5/COD值由0.004 提高到0.034。用接触氧化反应器处理经水解酸化处理后的废水，处理效果比较稳定，COD平均去除率达35.5%；3 研究了Fenton反应中各影响因子对废水COD去除率、BOD5/COD的影响并分析其作用机制，确定了最佳条件：初始pH为4.0，H2O2/Fe2+(摩尔浓度比)为20，H2O2/COD（质量浓度比）为1，反应时间为2 个小时。此条件下，废水的COD去除率约为40%，BOD5/COD值从0.002～0.003 提高至0.15～0.2，可生化性得到很大提高。本论文的主要创新点在于：1 以成分复杂、水质变化大的气井钻井废水为研究对象，从理论BOD 和表观BOD 两方面对水解酸化过程中废水可生化性的变化进行了分析；2 对Fenton 试剂改善钻井废水可生化性的过程、主要影响因素进行了比较详细的考察。本论文的研究成果，可为生物法处理钻井废水的深入研究提供理论依据。Drilling wastewater is produced in the process of oil-gas well drilling,because of its complicated composition, high concentrate of organic compound andsuspended solid, high chroma, levity of water quality and decentralization ofdischarge point, it pollutes environment seriously if discharged without treatment.With the development of petroleum industry and the issuing of more strict laws forenvironmental protection, it has been paid more and more attention on drillingwastewater treatment. It is of great importance for the sustainable development ofoil-gas well drilling to treat drilling wastewater by economical and effective methods.In this paper, drilling wastewater of Mo No.153 well in Suining was studied asthe main object. On the basis of research on pre-treatment with flocculant andbiological treatment, and according to the character of poor biodegradability, thedrilling wastewater was treated by hydrolytic acidification and Fenton’s reagent toimprove its biodegradability. The process and mechanism of biodegradabilitychanging were investigated. The primary conclusions are:1 It is effective to treat drilling wastewater with mixing PFS and PAC asflocculant. The removal rates of COD came up to 75% under optimal conditions, thesedimentation rate of flocculation is rapid, and the pH value of treated water remainedneutral;2 The biodegradability of drilling wastewater was highly improved afterhydrolytic acidification process. The theoretic BOD5 of drilling wastewater increasedby 22 times and its detected BOD5/COD ratio increased from 0.004 to 0.034 afterhydrolytic acidification for 48 hours. The wastewater after hydrolytic acidificationwas treated by biological contact oxidation reactor. Stable treatment performance was achieved, and the average removal rates of COD came up to 35.5%;3 The effects of various affection factors on the removal efficiency of COD andBOD5/COD radio in treating drilling wastewater by Fenton’s reagent wereinvestigated and the mechanism was analyzed. The optimal conditions were: initialpH of solution was 4.0, the molar ratio of H2O2 and Fe2+ was 20, the concentrationratio of H2O2 and COD was 1 and the reaction time was 120 min. Under the aboveconditions, the removal efficiency was about 40% and the ratio of BOD5 and CODincreased from 0.002 ¡« 0.003 to 0.15 ¡« 0.2. The biodegradability of drillingwastewater was greatly improved.The innovations of this thesis are:1 The drilling wastewater was taken as the research object which hascomplicated composition and variational water quality, and the changes ofbiodegradability were analyzed from theoretic BOD and detected BOD aspects duringhydrolytic acidification process;2 The biodegradability changing process and primary affection factors of drillingwastewater treating by Fenton’s reagent were investigated.The results of this study could provide theoretic foundation for further researchon biological treatment of drilling wastewater.

Stable isotopic compositions in Australian precipitation

Stable deuterium (delta D) and oxygen-18 (delta O-18) isotopes in 1962 to 2002 precipitation from the seven Australian stations of the Global Network of Isotopes in Precipitation (GNIP) were used to investigate isotope characteristics including temporal and spatial distributions across different regions of Australia. On the basis of 1534 samples, the local meteoric water line (LMWL) was established as delta D = 7.10 delta O-18 + 8.21. delta O-18 showed a depletion trend from north and south to central Australia (a continental effect) and from west to east. Precipitation amount effects were generally greater than temperature effects, with quadratic or logarithmic correlations describing delta/T and delta/P better than linear relationships. Nonlinear stepwise regression was used to determine the significant meteorological control factors for each station, explaining about 50% or more of the delta O-18 variations. Geographical control factors for delta O-18 were given by the relationship delta O-18 (parts per thousand) = -0.005 longitude (degrees) - 0.034 latitude (degrees)-0.003 altitude (m) - 4.753. Four different types of d-excess patterns demonstrated particular precipitation formation conditions for four major seasonal rainfall zones. Finally, wavelet coherence (WTC) between delta O-18 and SOI confirmed that the influence of ENSO decreased from east and north to west Australia.

Identification of high-lying odd energy levels of uranium by resonant ionization mass spectrometry

Single-colour and two-colour multiphoton resonant ionization spectra of uranium atom were studied extensively with a Nd: YAG laser-pumped dye laser atomic beam apparatus time-of-flight mass spectrometer in our laboratory. The energy locations of high-lying odd-parity levels in the region 33 003-34 264 cm(-1),mearured by a two-colour three-step ionization technique, were reported here. The angular momentum quantum number J was uniquely assigned for these levels by using angular momentum selection rules.

CRYSTAL-STRUCTURE AND THERMODYNAMIC PARAMETERS OF NYLON-1010

WAXD, SAXS, FTIR, DSC and density techniques have been used to investigate the crystal structure, crystal density rho(c), amorphous density rho(a), equilibrium heat of fusion DELTAH(m)degrees and equilibrium melting temperature T(m)degrees. By extrapolating the straight lines in the FTIR absorbance against density plot to zero intensity, rho(c) and rho(a) were estimated to be 1.098 and 1.003 g/cm3 respectively. The rho(c) obtained was too low in value. From X-ray diffraction patterns of uniaxially oriented fibres, the crystal structure of Nylon-1010 was determined. The Nylon-1010 crystallized in the triclinic system, with lattice dimensions: a = 4.9 angstrom, b = 5.4 angstrom, c = 27.8 angstrom, alpha = 49-degrees, beta = 77-degrees, gamma = 63.5-degrees. The unit cell contained one monomeric unit, the space group was P1BAR, and the correct value of rho(c) was 1.135 g/cm3. The degree of crystallinity of the polymer was determined as about 60% (at RT) using Ruland's method. SAXS has been used to investigate the crystalline lamellar thickness, long period, transition zone, the specific inner surface and the electron density difference between the crystalline and amorphous regions for Nylon-1010. The analysis of data was based upon a one-dimensional electron-density correlation function. DELTAH(m)degrees was estimated to be 244.0 J/g by extrapolation of DELTAH(m)degrees in the plot of heat of fusion against specific volume of semicrystalline specimens to the completely crystalline condition (V(sp)c = 1/rho(c)). Owing to the ease of recrystallization of melt-crystallized Nylon-1010 specimens, the well-known Hoffman's T(m)-T(c) method failed in determining T(m)degrees and a Kamide double extrapolation method was adopted. The T(m)degrees value so obtained was 487 K.

高纯氧化钬的电感耦合等离子体原子发射光谱分析及光谱干扰的校正

本文提出了以PGS-2型平面光栅摄谱仪与Plasma Therm ICP-5000D射频发生器联用,乙醇溶液预去溶进样方法,直接同时测定高纯氧化钬中5个稀土杂质元素的方法,并讨论了基体浓度对分析方法检出限的影响和光谱干扰及其校正。当样品溶液中稀土总浓度为5mg/ml时,测定下限分别为铽0.003％,镝、铒和铥0.002％,钇0.0003％。其相对标准偏差为2.8％～7.4％。

高纯金属镨的电感耦合等离子体原子发射光谱分析

某些稀土杂质对高纯金属镨的冶炼与性质有很大影响,因此需建立准确可靠的分析方法。镨的ICP光谱极为复杂,本文除用乙醇预去溶进样方式以提高分析灵敏度外,还研究了基体用量和稀土元素间的光谱干扰和校正方法。得出当样品中稀土总浓度为5mg/mL时,可直接同时测定纯度>99.99%的高纯金属镨中的镧、铈、钕、钐和钇,测定下限分别为镧、钕和钐0.002%,铈0.003%,钇0.0005%;其相对标准偏差分别为2.2%,6.2%,3.6%,1.4%和

高纯金属镨中痕量稀土杂质的电感耦合等离子体原子发射光谱分析及光谱干扰的校正

本文提出了PGS-2型平面光栅光谱仪（色散率0.18纳米，二级光谱）与Plasma Therm ICP-5000D射频发生器联用，乙醇预去溶方式进样，同时直接测定高纯金属镨中5个痕量稀土杂质元素的方法。并讨论了基体浓度对检出限的影响以及光谱干扰及其校正方法。当样品溶液中镨的浓度为5毫克/毫升时，测定下限分别为镧、钕和钐0.002%，铈0.003%和钇0.0005%。获得了良好的实验结果，并相对标准偏差为1.2-6.2%。

菲律宾蛤仔（Ruditapes philippinarum)能量代谢的研究

能量代谢指动物在进行生理活动(如摄食、消化以及动物的活动等)时所消耗能量的总和，一般以动物的呼吸率利排泄率来估计动物的能量代谢。其主要研究内容是闸明生物能量代谢的基木规律以及与环境闪子的关系。菲律宾蛤仔(Ruditapesphil ippmarum)是我国一种重要的养殖贝类，关于其能量代谢的研究却较少，这种状况妨碍了菲律宾蛤仔养殖生态理论的完善和养殖技术的提高。本研究主要对菲律宾蛤仔呼吸率和排泄率的基本规律(能量代谢与体重的关系、能量代谢的昼夜变化)及其与环境因子(饵料浓度、水温、栖息底质环境)的关系进行探讨。研究结果如下：1．不同体重菲律宾蛤仔代谢率小同。实验川菲律宾蛤仔分三种大小：l(干肉重为0．07-0．14g)、ll(干肉重0．27-0．34g)、III(干肉重0．45～0．63g)。温度包括：26℃(八月)、20℃(十月)、1 5℃(十二月)、9℃(一月)。实验共设四个饵料浓度：2．28±0．25，6．454±0．44，10．284±0．82，15．414±1．56mgTPM／L(TPM，总颗粒物)，饵料中POM(颗粒有机物)含量都为4．68±1．64 mg/L。常温下菲律宾蛤仔代谢率随着体重的增大而增大。15℃、20~C、26℃时蛤仔呼吸率与干肉重呈明显的幂函数关系R=aW~b，a值变动范围为0．1076-0．3309；b值变动范围为0．239l～0．8381；蛤仔排泄率与干肉重也呈明显的幂函数关系N=aW~b，a值变动范围为14．213～68．362：b值变动范围为0．3673-1．1 532。9℃(饵料浓度为2．28±0．25mgTPM／L)、20℃(饵料浓度为10．284-0．82mgTPM／L)、26℃(饵料浓度为6．454±0．44mgTPM／L)时不同体重蛤仔氧氮比差异显著，其它情况下不同体重蛤仔氧氮比差异不显著。2．常温下菲律宾蛤仔代谢率受饵料浓度的影响，不同大小蛤仔受饵料浓度的影响程度不同。I组蛤仔呼吸率受饵料浓度的显著影响，II组III组蛤仔呼吸率只在9℃(一月)和26~C(八月)时受饵料浓度的显著影响。26℃时影响最显著，26℃时I组蛤仔在饵料浓度为2．28±0．25，6．45±0．44，l0．28±0．82，15．4l±1．56mgTPM／L时呼吸率分别是O．086，0．146，0．073，0．093(mlO_2／h)；ll组蛤仔在上述浓度饵料中呼吸率分别是0．138，0．214，0．J 26，0．12l(mlO_2／h);III组蛤仔在上述浓度饵料中呼吸率分别是0．129，0．266，0．186，0．192(mlO_2／h)。菲律宾蛤仔呼吸率在饵料浓度为6．45±0．44 mgTPM／L时最高，蛤仔呼吸率在其它饵料浓度时都会降低。菲律宾蛤仔排泄率在饵料浓度为10．28±0．82 mgTPM／L和15．4l士1．56mgTPM／L时显著高于其它浓度组，9℃时这种趋势更明显，9℃时饵料浓度为2．28±0．25，6．454±044，lO．284±0．82，15．41±1．56mgTPM／L中I组蛤仔排泄率分别是4．297，2．874，8．003，6．658(μgNH_3-N／h)；II组蛤仔在上述浓度饵料中排泄率分别是4．011，3．609，10．427，12．732(μgNH_3-N／h)；III组蛤仔在上述浓度饵料中排泄率分别是2．28 l，6．452，10．283，15．417(μgNH_3-N／h)。3．菲律宾蛤仔代谢率受自然温度的显著影Ⅱ向。I组蛤仔在9℃、15℃、20℃、26℃时呼吸率平均为0．057，0．085，0．039，O．099；II组蛤仔在上述四个温度中呼吸率平均为0．08，O．128，0．089，0．149(mlO_2／h)，I组和II组蛤仔在9℃和20~C时呼吸率较低，在26℃时呼吸率最高。III组蛤仔在上述四个温度中呼吸率平均为0．09，O．1 59，O．143，O．193(mlO_2／h)，在9℃时llI组蛤仔呼吸率显著低于其它温度组。温度为9℃、15℃、20℃、26℃时l组蛤仔排泄率平均为5．458，13．169，4．946，11．138(μgNH_3-N／h)：II组蛤仔在上述温度中排泄率平均为7．695，23．578，8．319，23．90l(μgNH_3-N／h)；III组蛤仔在上述温度中排泄率平均为11．738，27．443，15．658，35．407(μgNH_3-N／h)，蛤仔排泄率在15℃和26℃时均高于9℃和20℃。4．摄食状态与饥饿状态菲律宾蛤仔代谢率有明显不同。26℃时蛤仔静止状态呼吸率平均为0．336(m102／g干重．h)，摄食状态呼吸率平均为0．656(ml0_2干重．h)，摄食状态呼吸率比静止状态平均升高了0 32(ml0_2／g干重．h)；26℃时蛤仔静止状态排泄率平均为39．471(μgNH_3-N／g干重．h)，摄食状态排泄率平均为88．08(μgNH_3-N／g干重．h)，摄食状态排泄率比静止状态排泄率平均升高了48．6(μgNH_3-N／g干重．h)。摄食状态代谢率平均是静止状态的2～3倍。根据摄食引起的呼吸率和排泄率升高量得出每氧化产生lμgNH_3-N需0_2量平均为7．05μl。5．人工控制温度对菲律宾蛤仔代谢率有明显影响。不同大小蛤仔受温度的影响程度不同。在温度5℃、10℃、l 5℃、20℃、26℃，I组和II组蛤仔呼吸率都随着温度的升高而升高，在10℃～l5℃和20℃～26℃这二个温度变化范围内呼吸率变化最大，在20℃～26℃时I组蛤仔呼吸率变动范围为O．85～1．04(m10_2／g干重．h)、II组蛤仔变动范围为0．57～0．86(ml0_2／g干重．h)。III组蛤仔呼吸率只在5℃～l0℃时明显增高，变动范围为0．09～0．5l(m10_2／g干重．h)，在10℃～26℃范围内变化不大。I组和II组蛤仔排泄率随着温度的升高而升高，变动幅度较大，在5℃～26℃范围内其排泄率变动范围为10．32～81．53(μgNH_3-N／g干重．h)；而 III组蛤仔排泄率只在5℃～15℃时随着温度的升高而升高，其排泄率变动范围为6．75～23．77(μgNH_3-N/g干重．h)，在15℃～26℃范围内几乎不变。III组蛤仔的适温范围比I组和II组蛤仔广。菲律宾蛤仔在5℃和10℃时氧氮比变化明显，变动范围为2．76～11．44，在15～26℃时变化不大。6．菲律宾蛤仔代谢率有明显的日节律性，呈正弦曲线型变化。蛤仔夜问代谢率明显升高。I组蛤仔夜间呼吸率平均为0．867(m10_2／g干重．h)，白天呼吸率平均为O．504(m10_2／g干重．h)；II组蛤仔夜间呼吸率平均为0．438(m10_2／g干重．h)，白天呼吸率平均为0．36l(m102／g干重．h)；III组蛤仔夜间呼吸率平均为0．409(m10_2／g干重．h)，白天呼吸率平均为0．252(m102／g干重．h)。在22：00-23：00菲律宾蛤仔呼吸率最高。7．底质环境对菲律宾蛤仔的代谢率有明显影响。在饥饿状态下菲律宾蛤仔在泥沙底质中呼吸率平均为l 406(m10_2／g干重h)，在无泥沙环境中呼吸率平均为O．963(ml0_2／g干重．h)；摄食状态下菲律宾蛤仔在泥沙底质中呼吸率平均为1．59l(m102／g干重．h)，在无泥沙环境中呼吸率平均为1．115(m10_2／g干重．h)。在饥饿状态下菲律宾蛤仔在泥沙底质中排泄率平均为78．934(μgNH_3-N／g 干重．h)，在无泥沙环境巾排泄率平均为45．043(μgNH_3-N／g干重．h)；摄食状态下菲律宾蛤仔在泥沙底质中排泄率平均为87．12l(μgNH_3-N／g干重．h)，在无泥沙底质中排泄率平均为58．354(μgNH_3-N／g干重．h)。蛤仔在泥沙环境中呼吸率和排泄率都明显升高。

一种用于异步电机效率优化的混合搜索方法

针对异步电机效率优化问题,提出了一种混合搜索方法。该方法起始于模糊自适应搜索,然后切换至黄金分割法以获取确定收敛速度。这样的搜索步骤能够降低转矩波动,避免在最优点附近发生振荡。利用一个包含铁损和机械损耗的异步电机模型,对该方法进行了矢量控制下的性能验证。仿真结果验证了该方法的有效性。

加权模糊相对熵在电机转子故障模糊识别中的应用

提出了一种基于加权模糊相对熵的电机转子故障模糊识别方法。该方法将加权思想引入到模糊相对熵,用于识别电机转子故障严重程度。加权方法的引入增加了信息量丰富的符号区间的模糊相对熵占全部区间模糊相对熵的比重,可以更充分、合理地利用该区间的故障信息进行故障识别。电机转子断条故障诊断仿真实验结果表明,提出的方法有效地实现了电机故障的定量分析,能够准确地识别出电机转子故障的严重程度,使算法的鲁棒性得到了改善,故障分类的可靠性及准确程度得到了提高。

改进的符号时间序列分析方法及其在电机故障诊断中的应用

提出了一种改进的基于符号时间序列分析的电机异常探测方法,该方法自适应地将符号序列中出现符号最多的符号区间重新划分为2个新的符号区间,使得数据密集区间可以分配到相对更多的符号,而数据稀疏区间则分配到较少的符号,提高了符号对于信号变化的灵敏度。电机转子断条故障的诊断实验结果表明:该方法较平均划分区间的方法对于电机异常诊断有着更高的灵敏度以及更好的鲁棒性和可靠性。

基于工业无线技术的非侵入式电机故障诊断系统

介绍一种适用于中小型电机的在线监测与故障诊断系统,系统采用无线传感器网络技术构建电机在线监测通信平台,利用非侵入电机电流信号特征分析技术,实现了电机运行状态的在线监测和电机转子断条、匝间短路等典型故障的在线诊断,为中小型电机的在线监测与能源管理提供了一种低成本解决方案。

黄骅坳陷大港探区油气资源潜力与资源结构预测

Facing the problems that Dagang region of Huanghua Depression has high exploration degree and its remaining resource potential and structure are not clear, the theory of Petroleum Accumulation System (PAS) is applied to divide and evaluate the oil/gas systems quantitatively. Then, the petroleum accumulation systems are taken as units to forecast and analyse the oil/gas resources and their structure using statistical methods of sampling analysis of discovery process model and generalized pareto distribution model. The exploration benefit of the unit is estimated using exploration simulation methods. On the basis of the above study, the resource potential of Huanghua Depression is discussed.Huanghua Depression can be diveded into four petroleum accumulation systems, i.e. North PAS5 Middle Qibei PAS, Middle Qinan PAS and South PAS. Each PAS can be diveded futher into several sub- PASs. Using the basic princple of Analytical Hierarchy Process, the method of quantitative evaluation of PAS is established. Then the elements and maturity of PAS are evaluated quantitatively.Taking migration and accumulation units and sub-PASs as prediction units, sampling analysis of discovery process model and generalized pareto distribution model are applied comparatively to forecast the resource structure of eight migration and accumulation units in six PASs of medium-high exploration degree. The results of these two methods are contrasted and analyzed. An examination of X2 data of these two models from exploration samples shows that generalized pareto distribution model is more effective than sampling analysis of discovery process model in Huanghua Depression. It is concluded that minimum and maximum size of reservoir and discovery sequence of reservoirs are the sensitive parameters of these two methods.Aiming at the difficult problem of forecast in low exploration degree, by analysis of relativity between resource parameters and their possible influential geological factors, forecast models for resource parameters were established by liner regressing. Then the resource structure is forecasted in PASs of low exploration degree.Based on the forecast results, beginning with the analysis of exploration history and benefit variation, the exploration benefit variation of the above PASs is fitted effectively using exploration simulation method. The single well exploration benefit of remaining oil resource is also forecasted reasonably.The results of resource forecast show that the total oil resources ofHuanghua Depression amount to 2.28 b illion ton. By the end o f 2 003, the accumulative total proved oil reserve is 0.90 billion ton and the remaining oil resources is 1.38 billion ton. The remaining oil resource is concentrated in Kongdian-Dengmingshi, Banqiao-Beidagang, Qidong-Yangerzhuang and Baidong-Qizhong sub-PASs.

Formation of the V center on H-type zeolites with thermal treatment

The effect of thermal treatment on H-MCM-22 and H-ZSM-5 zeolites was investigated using the electron spin resonance technique. A six-line signal (denoted as A, g = 2.048, A = 22. 15 G) was detected on H-MCM-22 after He purging at high temperatures, whose intensities increased with the treating temperature. The same signal was also found on H-ZSM-5 zeolites with different crystal sizes. The paramagnetic center was identified as a V center, namely, a hole of an electron trapped on an oxygen atom bonding to a nearby aluminum atom. These signals appeared only on a dealuminated sample or a sample concomitantly with dealumination. The formation of the hole might involve an electron transferring from the lattice oxygen to a nonframework aluminum species, and the hyperfine splitting is caused by the interaction between the electron hole locating on the p orbit of oxygen and the framework aluminum bonding with the oxygen. The signal disappeared after the sample was exposed to air or oxygen at room temperature. However, the process was reversible. A new set of signals (denoted as B, g(1) = 2.008, g(2) = 2.003, g(3) = 1.9985) was observed after oxygen adsorption on the H-MCM-22 pretreated with He at 973 K or He purging at 973 K on the H-MCM-22 pretreated with oxygen at 813 K, which was attributed to the O- species.