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11.
12.
Sodium chlorite (SC) is an effective sanitizer for inhibiting microbial growth. This investigation was conducted to determine the efficacy of SC as a browning control agent for use on fresh-cut apple slices, applied alone, or in conjunction with organic acids. Additionally, the authors compared the efficacy of SC to that of acidified sodium chlorite (ASC) and to several other salts and examined the effect of pH and several different organic acids on efficacy of SC. The fresh-cut apple slices were dipped in treatment solutions for 1 min, then drained and placed in plastic containers at 20 °C for 24 h, and finally stored in polyethylene bags at 5 °C for 2 weeks. Color was measured periodically during storage. Lightness (L) values for all treated and control samples measured at 4 h, 24 h, and 2 weeks of storage were compared to L value for untreated samples measured immediately after cutting. Percent decrease in L-values was calculated for each sample at each time interval. Apple slices treated in ASC or SC solution had a significantly smaller decrease in L value indicating less browning than those treated in citric acid or water control at 4 h (P < 0.01), and with the exception of 1 g L−1 ASC and 0.1 g L−1 SC, all other ASC and SC treated slices still had significantly less browning than those for the water control (P < 0.01) at 24 h. After 2 weeks of storage, only SC (0.5–1.0 g L−1), sodium bisulfite (0.5 g L−1) and calcium l-ascorbate (10 g L−1) continued to inhibit browning. Treatment with 0.5 g L−1 SC and pH adjusted in the range from 3.9 to 6.2 using citric acid (CA) reduced browning more effectively than 0.5 g L−1 SC without pH adjustment. Two organic acids, salicylic acid and cinnamic acid, when added to SC solution, were found to achieve even better inhibition of browning than CA at the same pH value. 相似文献
13.
西湖凹陷古近系及新近系储层砂岩自生高岭石分布特征及形成机制 总被引:1,自引:0,他引:1
在西湖凹陷古近系及新近系储层砂岩中,自生高岭石是含量仅次于碳酸盐的第二大自生矿物,主要是长石等铝硅酸盐矿物溶解的产物;自生高岭石含量与砂岩碎屑中的长石含量有着明显的负相关性,自生高岭石含量在凹陷中呈现的东西分带、南高北低的分布特点与成岩作用过程中有机酸和大气水对长石等铝硅酸盐的溶解作用有关,其中有机酸作用明显强于大气水。西湖凹陷平湖组在西斜坡具有比中央反转带明显高的自生高岭石含量,南部地区相对北部地区具有相对较高的高岭石含量,说明西斜坡平湖组和南部地区具有更好的次生孔隙形成条件,其储层质量更好。 相似文献
14.
粘土矿物是低渗砂岩储层的主要胶结物,对储层物性及开发过程中储层物性变化趋势有着重要的影响和控制作用。另外,粘土矿物也蕴含着大量沉积环境介质的物理化学信息,认识其自然规律,可以有效地指导预测有利储层,认识和改造油层。以鄂尔多斯盆地砂岩储层中的粘土矿物为研究对象,探讨分析粘土矿物对低渗储层性质的影响,该研究对含油气盆地低渗储层有效开发具有一定的参考价值。 相似文献
15.
Removal of SO2 and NO from flue gas by wet scrubbing using an aqueous NaClO2 solution 总被引:15,自引:0,他引:15
This study used a NaClO2/NaOH solution as the additive/absorbent to determine the extent of NOx removal in a wet scrubbing system. A combined SOx/NOx removal system was also tested. The experiments were performed in a bench-scale spraying sieve tray wet scrubber in a continuous mode. The operating variables included NO and SO2 concentrations, L/G ratio, molar ratio, and initial pH.
The results of the individual DeNOx experiments show that the maximum DeNOx efficiencies ranged from 3.1 to 12.6%. The results of the combined DeSOx/DeNOx experiments show that the maximum DeNOx and DeSOx efficiencies ranged from 36.6 to 71.9% and from 89.4 to 100.0%, respectively. The major parameters affecting NOx removal efficiencies are the L/G ratio and the dosage of additive. The major parameter influencing DeSOx efficiencies is the L/G ratio. 相似文献
16.
S. Fröhlich J. Redfern L. Petitpierre J.D. Marshall M. Power P.V. Grech 《Journal of Petroleum Geology》2010,33(1):3-18
This paper assesses the diagenetic history of potential fluvial hydrocarbon reservoir rocks deposited within incised valley systems of the Lower Carboniferous Marar Formation in western Libya. Outcrop data were collected in the Tinedhan Anticline, located at the southern margin of the Ghadames Basin. Four discrete intervals with channelized sandstones were identified in a section dominated by alternating offshore mudstones and shallow-marine clastics. The incised channels were cut during major sea-level lowstands, and filled by fluvial sandstone packages up to 50 m thick. Fifty-eight samples from four different localities, representing three lowstand systems tracts, were analysed to obtain a statistically meaningful mineralogical and compositional dataset. In addition to burial compaction, three main diagenetic events influenced the reservoir quality of the sandstones. Firstly, early eodiagenesis involved kaolinitization of plagioclase grains. This began before subsequent calcite cementation, probably as a result of flushing by meteoric pore-waters. The deformation of kaolinite during later compaction resulted in the formation of pseudomatrix which further reduced porosity and permeability. Kaolinite is commonly transformed to illite at temperatures above 140°C in the presence of K-feldspar. Although K-feldspar was recorded in the samples, no illite was observed, suggesting that the Lower Carboniferous strata in the study area were not buried in excess of approximately 3.5 km. The second diagenetic phase was the precipitation of calcite cement, present either dispersed throughout the sandbodies or as concretions up to 2 m across, in both cases reducing reservoir quality. The high intergranular volumes (IGV) of calcite-cemented sandstones (ranging between 35% and 40%) suggest that cementation occurred at burial depths of <500 m. Sandstones without calcite cement have lower IGV of between 17% and 25% as a result of mechanical and chemical compaction. Stable C and O isotope analysis of the calcite cement also supports precipitation at shallow burial depths, indicating a meteoric pore-water source for the calcite. The third and final diagenetic stage was partial chloritisation of kaolinite during meso-diagenesis. The elevated temperatures required for this transformation indicate burial to a minimum depth of approximately 2.5 km, which is consistent with the compaction data. Despite these diagenetic effects, the fluvial sandstones have an average porosity of 12%, with a range from 0.5% up to 25%. Permeability measurements on four sandstone samples indicate that the development of pseudomatrix did not reduce permeability significantly. 相似文献
17.
J. M. Huggett S.D. Burley F. J. Longstaffe S. Saha M. J. Oates 《Journal of Petroleum Geology》2015,38(4):383-409
Reservoir sandstones in the Mid‐ and South Tapti gas fields in the Surat Depression (Mumbai Offshore Basin, western India) have been investigated using a range of petrographic techniques, isotope geochemistry and basin modelling. Authigenic chlorite is abundant in the shallow‐marine sandstones of the Miocene Mahim Formation, a major reservoir rock in the Mid‐ and South Tapti fields, which are described here in terms of their quality and diagenetic characteristics. The sandstones are currently at burial depths of between ~1500 and 2800m. The authigenic chlorite has had a significant impact on the resulting reservoir quality of the sandstones and is interpreted to have originated as odinite clay of the verdine facies that replaced faecal or pseudo‐faecal pellets, together with volumetrically small but abundant grain coatings and grain rims, and formed at the site of major riverine iron influx onto the shallow‐marine shelf during periods of relatively low sea level. Pellets have been variably compacted to form pseudomatrix. Reservoir sandstones from similar depositional settings on the west coast of India or other sub‐tropical settings are likely to exhibit comparable diagenetic effects on reservoir quality. Compositionally, the chlorite is the iron‐rich form known as chamosite. The chemistry of all the chlorite morphologies is the same in all studied samples. Oxygen isotope analyses of carbonate cements in the Mahim Formation sandstones have provided an approximate temperature framework for diagenesis of the non‐carbonate cements. Oxygen isotope results for the chlorite, however, suggest much higher temperatures than its position in the paragenetic sequence would warrant. These results suggest that the clay formed first as 1:1 layer clays, in this case odinite, which were then transformed to Fe‐chlorite as burial depths and temperatures increased. Reservoirs in the Mahim, Daman and Mahuva Formation sandstones are thus greatly influenced by the diagenesis of authigenic chlorite and locally by the precipitation of carbonate cements. Reservoir quality is good where thick, continuous chlorite rim cements are present and where chlorite pellets are sufficiently indurated for them not to be compacted. Chlorite rim cements have reduced the extent of quartz overgrowth cementation in the sandstones. 相似文献
18.
管俊芳 《华北水利水电学院学报》2000,21(2):41-45
对周口和通许两地区 4口井砂岩的薄片观察、多种测试、分析 ,发现砂岩中石英的增生可分窄边型、宽边型和自形边型 3种 ,增生石英的发育情况与砂岩的类型、成分等密切相关 .宽边和自形边型增生石英形成的温度一般在 1 0 0℃~ 1 50℃ .硅质物来源主要是孔隙内原生孔隙水供给、成岩过程中泥层蒙脱石→伊利石转化供给、或长石的溶解作用供给 .成岩中晚期有机质向烃转化发生脱羧基作用 ,地下流体变为酸性 ,促进了长石颗粒的溶解 ,增加了硅物质供给 .通过研究该地区内砂岩石英的增生 ,对进一步分析区内砂岩的孔隙演化、次生孔隙形成、砂岩储层物性等具有重要意义 相似文献
19.
通过对大鼠90d喂养试验,研究了ClO2及其副产物ClO2和ClO3混合溶液对大鼠血液学指标的影响,结果表明,大鼠血液学指标,即白细胞计数(WBC)和血红蛋白(Hb)方差分析结果显示,CIO2混合液对其均未产生影响(p>0.05);对谷-丙转氨酶(ALT)、总蛋白(TP)、白蛋白(ALB)和球蛋白(GLO)的方差分析表明,其对照组和高剂量组雌雄相比无显著性差异(p>0.05)。 相似文献
20.
Experiments of simultaneous removal of SO2 and NO from simulated flue gas, using NaClO2 solution as the absorbent, were carried out in a self-designed bubble reactor, and high simultaneous removal efficiencies
of SO2 and NO were obtained under the optimal experimental conditions. The mechanism of simultaneous removal based on NaClO2 acid solutions was proposed by analyzing the removal products. Possibility and limitation of the desulfurization and denitrification
using NaClO2 acid solutions were calculated by thermodynamic methods. Experimental results of reaction kinetics for simultaneous desulfurization
and denitrification indicated that the oxidation-absorption processes of SO2 and NO were divided into two zones, namely the fast and slow reaction zones. In the slow reaction zones both were zero order
reactions, and in the fast reaction zones, the reaction order, rate constant and activation energy of SO2 reaction with absorbent were 1.4, 1.22 (mol·L−1)−0.4·s−1 and 66.25 kJ·mol−1, respectively, and 2, 3.15×103 (mol·L−1) −1·s−1, and 42.50 kJ·mol−1 for NO reaction, respectively.
Supported by the National High-Tech Research and Development Program of China (“863” Project) (Grant No. 2007AA061803) 相似文献