Mathematical modeling of mixed convective MHD Falkner-Skan squeezed Sutterby multiphase flow with non-Fourier heat flux theory and porosity

In a wide variety of mechanical and industrial applications,e.g.,space cooling,nuclear reactor cooling,medicinal utilizations(magnetic drug targeting),energy generation,and heat conduction in tissues,the heat transfer phenomenon is involved.Fourier’s law of heat conduction has been used as the foundation for predicting the heat transfer behavior in a variety of real-world contexts.This model’s production of a parabolic energy expression,which means that an initial disturbance would immediately affect the system under investigation,is one of its main drawbacks.Therefore,numerous researchers worked on such problem to resolve this issue.At last,this problem was resolved by Cattaneo by adding relaxation time for heat flux in Fourier’s law,which was defined as the time required to establish steady heat conduction once a temperature gradient is imposed.Christov offered a material invariant version of Cattaneo’s model by taking into account the upper-connected derivative of the Oldroyd model.Nowadays,both models are combinedly known as the Cattaneo-Christov(CC)model.In this attempt,the mixed convective MHD Falkner-Skan Sutterby nanofluid flow is addressed towards a wedge surface in the presence of the variable external magnetic field.The CC model is incorporated instead of Fourier’s law for the examination of heat transfer features in the energy expression.A two-phase nanofluid model is utilized for the implementation of nano-concept.The nonlinear system of equations is tackled through the bvp4c technique in the MATLAB software 2016.The influence of pertinent flow parameters is discussed and displayed through different sketches.Major and important results are summarized in the conclusion section.Furthermore,in both cases of wall-through flow(i.e.,suction and injection effects),the porosity parameters increase the flow speed,and decrease the heat transport and the influence of drag forces.

Design of a Multifrequency Signal Parameter Estimation Method for the Distribution Network Based on HIpST

The application of traditional synchronous measurement methods is limited by frequent fluctuations of electrical signals and complex frequency components in distribution networks.Therefore,it is critical to find solutions to the issues of multifrequency parameter estimation and synchronous measurement estimation accuracy in the complex environment of distribution networks.By utilizing the multifrequency sensing capabilities of discrete Fourier transform signals and Taylor series for dynamic signal processing,a multifrequency signal estimation approach based on HT-IpDFT-STWLS(HIpST)for distribution networks is provided.First,by introducing the Hilbert transform(HT),the influence of noise on the estimation algorithm is reduced.Second,signal frequency components are obtained on the basis of the calculated signal envelope spectrum,and the interpolated discrete Fourier transform(IpDFT)frequency coarse estimation results are used as the initial values of symmetric Taylor weighted least squares(STWLS)to achieve high-precision parameter estimation under the dynamic changes of the signal,and the method increases the number of discrete Fourier.Third,the accuracy of this proposed method is verified by simulation analysis.Data show that this proposed method can accurately achieve the parameter estimation of multifrequency signals in distribution networks.This approach provides a solution for the application of phasor measurement units in distribution networks.

食管癌术后淋巴结状态对术后辅助治疗选择的预测价值

目的:分析食管癌患者术后的淋巴结状态对术后辅助治疗方案选择的预测价值及与预后的关系。方法:分析2007年1月至2010年12月河北医科大学第四医院354例食管癌根治术后患者,对其淋巴结各相关参数与术后辅助治疗进行预后分析。单因素生存分析采用Kaplan-Meier法和Log-rank检验,多因素生存分析采用Cox回归模型。结果:全组患者1、3、5年生存率分别为84.46%、64.12%和54.06%,中位生存期为86.49个月。N0、N1、N2、N3期患者的5年生存率分别为93.13%、55.50%、19.80%和3.45%,不同N分期之间的差异具有统计学意义(χ^2=225.161,P<0.001)。通过ROC曲线获取阳性淋巴结数目与清扫总淋巴结数目的比值(LNR)为分组界值8.51%将其分为两组并进行生存分析,LNR≤8.51%组及LNR>8.51%组患者的5年生存率分别为81.63%和23.40%,两组之间的差异具有统计学意义(χ^2=143.504,P<0.001)。单因素预后分析显示术后T分期、N分期、LNR、阴性淋巴结数目与患者的生存预后均相关(均P<0.05)。多因素预后分析显示术后N分期、LNR为生存预后的独立影响因素(均P<0.05)。N2组及LNR>8.51%组接受术后辅助治疗的患者生存显著优于单纯手术组(χ^2=12.609,P<0.001;χ^2=13.171,P<0.001)。联合N分期及LNR进行分析,在LNR>8.51%组的N2期患者接受术后辅助治疗组生存显著优于单纯手术组(χ^2=12.609,P<0.001)。结论:LNR可以协同N分期更好地提示预后并指导食管癌根治术后患者辅助治疗的选择。对N2期同时伴有高LNR的患者应该积极选择术后辅助治疗。

Preparation of composite poly(ether block amide)membrane for CO_2 capture

In this study, a poly（ether block amide） （Pebax 1657） composite membrane applied for COa capture was prepared by coating Pebax 1657 solution on polyacrylonitrile （PAN） ultrafiltration membrane. Ethanol/water mixture was used as the solvent of Pebax and the effects of ethanol/water mass ratios and Pebax concentration on the permeation properties of composite membrane were studied. To enhance the com- posite membrane permeance, the gutter layer, made from reactive amino silicone crosslinking with potydimethylsiloxane （PDMS）, was de- signed. The influence of crosslinldng degree of the gutter layer on membrane performance was investigated. As a result, a Pebardamino- PDMS/PAN multilayer membrane with hexane resistance was developed, showing CO2 permeance of 350 GPU and CO2/N2 selectivity over 50. The blend of polyethylene glycol dimethyl ether （PEG-DME） with Pebax as coating material was studied to further improve the membrane performance. After being combined with PEG-DME additive, CO2 permeance of the final Pebax-PEG-DME/amino-PDMS/PAN composite membrane reached 400 GPU above with CO2/Na selectivity over 65.

Zinc isotopic behavior of mafic rocks during continental deep subduction

Zinc isotopes may act as a new tool of tracking recycling of crustal materials that causes compositional heterogeneity of the mantle.This application relies on an investigation of Zn isotopic behaviors during slab subduction.In this study,we report Zn isotopic compositions for a suite of metabasalts(greenschists,amphibolites,and coesitebearing eclogites)from the Dabie Orogen(China),which were formed via the subduction of mafic rocks into different depths and up to>200 km.Three out of eight greenschists are characterized by lighterδ^(66)ZnJMC-Lyon(0.10‰-0.16‰)than those of global basalts(0.28‰±0.05‰),which may be caused by crustal assimilation of the protoliths by sedimentary rocks due to their extremely high ^(87)Sr/^(86)Sr(up to 0.7130)and lowεNd values(down to−12.3).The remaining greenschists have relatively low ^(87)Sr/^(86)Sr and theirδ66Zn values(0.21‰-0.38‰)overlap the ranges of amphibolites(0.18‰-0.32‰)and coesite-bearing eclogites(0.18‰-0.36‰).There is no correlation betweenδ^(66)Zn and sensitive indicators of dehydration(Rb/TiO_(2),Ba/Yb,and H_(2)O+),suggesting that no detectable Zn isotope fractionation has occurred during the deep subduction of mafic rocks even into>200 km,which is attributed to the limited loss of Zn during prograde metamorphism and dehydration.Thus,Zn isotopic compositions of the deeply subducted mafic rocks are inherited from their protoliths.Considering that these metamorphosed rocks have higherδ66Zn than that of the mantle value by up to 0.2‰,the recycled/subducted mafic crust can incorporate isotopically heavy Zn into the mantle.The subducted slabs may partially melt and generate a metasomatized mantle,resulting in changes of Zn isotopic composition of the hybridized mantle as have been observed in some mantle xenoliths and basaltic lavas.

Isolation and Identification of a High-pathogenicity Strepto- coccus suis Serotype 7 Strain

In order to diagnose the diseased pigs in a certain large pig farm in Binzhou City, Shandong Province, the dead piglets with joint swelling were subjected to necroscopy, and the pathogenic bacterium was isolated and identified. One Gram-positive Streptococcus was isolated. The strain was subjected to characteristic culture, microscopic examination and molecular biological identification, and resistance detection, animal regression experiment and mouse pathogenicity test were carried out. The results showed that the isolate was identified to be Streptococcus suis serotype 7, which was resistant to multiple drugs; and the pathogenicity test showed that the strain had high pathogenicity to pigs, resulting in neurosis on partial pigs, and the strain had no pathogenicity to Kunming and BALB/c mice but certain pathogenicity to CD1 mice.

Post-collisional lithosphere delamination of the Dabie-Sulu orogen

The consistence between the first rapid cooling time (226-219 Ma) of the untrahigh pressure metamorphic (UHPM) rocks in the Dabie Mountains and the formation time (205-220 Ma) of the syncollisional granites in the Qinling and Sulu areas suggests that the first rapid cooling and uplift of the UHPM rocks may be related to breakoff of subducted plate. Therefore the second rapid cooling and uplift (180-170 Ma) of the UHPM racks needs a post-colli-sional lithosphere delamination which resulted in the granitic magmatism with an age of about 170 Ma. In addition, the rapid rising of the Dabie dome in the early Cretaceous (130-110 Ma) and the corresponding large-scale magmatism in the Dabie Mountains need another litho-sphere delamination. The geochronology of the post-collis-ional mafic-ultramafic intrusions and geological relationship between the mafic-ultramafic intrusions and granites suggest that partial melting was initiated in the mantle, and then progressively developed in the crust, suggesting a mantle

Formation time of the big mantle wedge beneath eastern China and a new lithospheric thinning mechanism of the North China craton—Geodynamic effects of deep recycled carbon

High-resolution P wave tomography shows that the subducting Pacific slab is stagnant in the mantle transition zone and forms a big mantle wedge beneath eastern China. The Mg isotopic investigation of large numbers of mantle-derived volcanic rocks from eastern China has revealed that carbonates carried by the subducted slab have been recycled into the upper mantle and formed carbonated peridotite overlying the mantle transition zone, which becomes the sources of various basalts. These basalts display light Mg isotopic compositions(δ26 Mg = –0.60‰ to –0.30‰) and relatively low87 Sr/86 Sr ratios(0.70314–0.70564) with ages ranging from 106 Ma to Quaternary, suggesting that their mantle source had been hybridized by recycled magnesite with minor dolomite and their initial melting occurred at 300-360 km in depth. Therefore, the carbonate metasomatism of their mantle source should have occurred at the depth larger than 360 km, which means that the subducted slab should be stagnant in the mantle transition zone forming the big mantle wedge before 106 Ma. This timing supports the rollback model of subducting slab to form the big mantle wedge. Based on high P-T experiment results, when carbonated silicate melts produced by partial melting of carbonated peridotite was raising and reached the bottom(180–120 km in depth) of cratonic lithosphere in North China, the carbonated silicate melts should have 25–18 wt% CO2 contents, with lower Si O2 and Al2 O3 contents, and higher Ca O/Al2 O3 values, similar to those of nephelinites and basanites, and have higher εNdvalues(2 to 6). The carbonatited silicate melts migrated upward and metasomatized the overlying lithospheric mantle, resulting in carbonated peridotite in the bottom of continental lithosphere beneath eastern China. As the craton lithospheric geotherm intersects the solidus of carbonated peridotite at 130 km in depth, the carbonated peridotite in the bottom of cratonic lithosphere should be partially melted, thus its physical characters are similar to the asthenosphere and it could be easily replaced by convective mantle. The newly formed carbonated silicate melts will migrate upward and metasomatize the overlying lithospheric mantle. Similarly, such metasomatism and partial melting processes repeat, and as a result the cratonic lithosphere in North China would be thinning and the carbonated silicate partial melts will be transformed to high-Si O2 alkali basalts with lower εNdvalues(to-2). As the lithospheric thinning goes on,initial melting depth of carbonated peridotite must decrease from 130 km to close 70 km, because the craton geotherm changed to approach oceanic lithosphere geotherm along with lithospheric thinning of the North China craton. Consequently, the interaction between carbonated silicate melt and cratonic lithosphere is a possible mechanism for lithosphere thinning of the North China craton during the late Cretaceous and Cenozoic. Based on the age statistics of low δ26 Mg basalts in eastern China, the lithospheric thinning processes caused by carbonated metasomatism and partial melting in eastern China are limited in a timespan from 106 to25 Ma, but increased quickly after 25 Ma. Therefore, there are two peak times for the lithospheric thinning of the North China craton: the first peak in 135-115 Ma simultaneously with the cratonic destruction, and the second peak caused by interaction between carbonated silicate melt and lithosphere mainly after 25 Ma. The later decreased the lithospheric thickness to about70 km in the eastern part of North China craton.

Review of drought impacts on carbon cycling in grassland ecosystems

Grasslands play a key role in both carbon and water cycles.In semi-arid and arid grassland areas,the frequency and intensity of droughts are increasing.However,the influence of a drought on grassland carbon cycling is still unclear.In this paper,the relationship between drought and grassland carbon cycling is described from the perspective of drought intensity,frequency,duration,and timing.Based on a large amount of literature,we determined that drought is one of the most prominent threats to grassland carbon cycling,although the impacts of different drought conditions are uncertain.The effects of a drought on grassland carbon cycling are more or less altered by drought-induced disturbances,whether individually or in combination.Additionally,a new conceptual model is proposed to better explain the mechanism of droughts on grassland carbon cycling.At present,evaluations of the effects of droughts on grassland carbon cycling are mainly qualitative.A data fusion model is indispensable for evaluating the fate of carbon cycling in a sustainable grassland system facing global change.In the future,multi-source data and models,based on the development of single and multiple disturbance experiments at the ecosystem level,can be utilized to systematically evaluate drought impacts on grassland carbon cycling at different timescales.Furthermore,more advanced models should be developed to address extreme drought events and their consequences on energy,water,and carbon cycling.

Rb-Sr chronology and cooling history of the Renjiawan pyroxenite intrusion in North Dabie Terrane

A group of Rb-Sr ages, i.e. plagioclase-whole rock (WR) isochron age of (205±7) Ma,hornblende-WR isochron age of (164±10) Ma and biotite-WR isochron age of (123.4±1.2)Ma, for one pyroxenite sample from Renjiawan in North Dabie Terrane (NDT) are reported. According to the closure temperature of 600℃ for plageoclase and 300℃ for biotite, the Renjiawan pyroxenite should intrude into the NDT before 205 Ma, and the younger Rb-Sr ages may reflect the cooling history of the intrusion or reset by the very strong Cretaceous thermal event in NDT.

Composition of plagioclase in Dabie Early Cretaceous granitoids:influence of fractional crystallization on whole-rock Sr–Ca O correlations

Identifying melts of thickened lower continental crust from high Sr/Y rocks is very important to trace deep crustal processes. Recent studies on Dabie Early Cretaceous granitoids have revealed that melts derived from thickened lower continental crust have higher Sr/Ca O ratios and define a high Sr evolution trend compared with normal granitoids. Fractional crystallization of plagioclase can significantly change Sr and Ca O contents of melts, but its role in controlling the Sr/Ca O ratios of the melts is still unclear. This study gives a direct comparison of plagioclase compositions between normal granitoids and low-Mg adakitic rocks. On the basis of Sr–Ca exchange partition coefficient, discussions on effect of plagioclase crystallization on Sr/Ca O ratios of melts show that fractional crystallization of abundant plagioclase cannot significantly change Sr/Ca O ratios of granitic melts, which are inherited from their individual initial melts. High Sr/Ca O ratios indicate the absence of plagioclase in sources of granitic melts. Therefore, high Sr/Ca O correlation can be an important indicator to identify melts derived from thickened lower continental crust.

Sm-Nd age of syncollisional mafic-ultramafic intrusions in the Dabie Mountains

A Sm_Nd age of (228±42) Ma with initial ε Nd =-16.4 for the Renjiawan pyroxenite intrusion in the North Dabie terrane is reported. This age with another Sm_Nd age of (230±44) Ma for the Zhujiapu pyroxenite in the same terrane documents that the pyroxenite in the North Dabie terrane are formed during continental subduction time of the Yangtze craton in the Triassic.

农村土地两个三权分置的法律意义

两个"三权分置",实际上是有"两个分离":第一个分离是承包权和经营权的分离;第二个分离是资格权和使用权的分离。但是,承包权和资格权都是一个不清晰、不完整的权利,因此,当它在分离过程中进入交易环节时就会产生不确定性。无论是使用权还是经营权,在交易过程当中都会产生很大的交易成本,且估值困难,因为概念不清晰,如果这些权利要进入市场环节,因为确定性不强,依据这样一个模糊的基础来建构一个明确的法律秩序是比较困难的。

替加环素不敏感鲍曼不动杆菌的分子流行病学及耐药机制

为探讨替加环素不敏感鲍曼不动杆菌Acinetobacter baumannii的耐药机制,为院内感染控制及临床合理用药提供理论依据,采用琼脂稀释法和微量肉汤稀释法检测全国多中心12个城市20家医院临床分离的94株非重复的替加环素不敏感鲍曼不动杆菌的最低抑菌浓度(Minimum inhibitory concentration,MIC),应用多位点序列分型(Multilocus sequence typing,MLST)技术进行分子流行病学研究,应用eBURST软件对MLST结果进行分析;用PCR和测序技术分析常见耐药基因(bla_(OXA-40-like)、bla_(OXA-58-like)、bla_(OXA-23-like)、bla_(OXA-51-like)、bla_(NDM-1)),与替加环素耐药相关的外排泵调控基因adeR和adeS的突变位点、trm的突变位点。经检测94株鲍曼不动杆菌除对多粘菌素B 100%敏感、对米诺环素敏感率25.5%外,其他抗菌药物的敏感率均低于3.5%,亚胺培南和美罗培南敏感率均只有1.1%。MLST分型得到12种ST分型,以ST195(45株,47.9%)、ST208(19株,20.2%)和ST457(10株,10.6%)为主,eBURST分析发现其中8个ST型均属于克隆复合体92(Clonal Complex 92,CC92);99%菌株bla_(OXA-23-like)型碳青霉烯酶基因阳性;均未扩增出bla_(NDM-1)基因;外排泵调控基因adeR和adeS的检出率分别是73.4%和91.5%,Asp26Asn和Ala97Glu分别为adeR和adeS的高频突变位点;在12株鲍曼不动杆菌中检测到了adeS基因的ISAba1,以北部地区为主;trm基因均在第240位核苷酸发生缺失突变。综上所述,替加环素不敏感鲍曼不动杆菌对除多粘菌素B外的大多数抗菌药物具有很高的耐药性,AdeABC外排泵上游的双组分调控系统adeR和adeS的缺失和突变,trm缺失突变是导致鲍曼不动杆菌对替加环素敏感性降低的主要原因。

The oxygen cycle and a habitable Earth

As an important contributor to the habitability of our planet, the oxygen cycle is interconnected with the emergence and evolution of complex life and is also the basis to establish Earth system science. Investigating the global oxygen cycle provides valuable information on the evolution of the Earth system, the habitability of our planet in the geologic past, and the future of human life. Numerous investigations have expanded our knowledge of the oxygen cycle in the fields of geology,geochemistry, geobiology, and atmospheric science. However, these studies were conducted separately, which has led to onesided understandings of this critical scientific issue and an incomplete synthesis of the interactions between the different spheres of the Earth system. This review presents a five-sphere coupled model of the Earth system and clarifies the core position of the oxygen cycle in Earth system science. Based on previous research, this review comprehensively summarizes the evolution of the oxygen cycle in geological time, with a special focus on the Great Oxidation Event(GOE) and the mass extinctions, as well as the possible connections between the oxygen content and biological evolution. The possible links between the oxygen cycle and biodiversity in geologic history have profound implications for exploring the habitability of Earth in history and guiding the future of humanity. Since the Anthropocene, anthropogenic activities have gradually steered the Earth system away from its established trajectory and had a powerful impact on the oxygen cycle. The human-induced disturbance of the global oxygen cycle, if not controlled, could greatly reduce the habitability of our planet.

Carbonated Big Mantle Wedge Extending to the NE Edge of the Stagnant Pacific Slab:Constraints from Late Mesozoic-Cenozoic Basalts from Far Eastern Russia

It has been suggested that the carbonated mantle reflected by Mg-Zn isotopic anomalies of Cenozoic intraplate basalts from East Asia coincides with the stagnant West Pacific slab in the mantle transition zone.However,the northern boundary of such carbonated domain beneath East Asia is uncertain.Late Mesozoic-Cenozoic intraplate basalts are widespread in far eastern Russia and thus provide an opportunity to examine this issue.Here we report major-trace element contents and Sr-NdMg-Zn isotopic compositions for 9 Late Mesozoic-Cenozoic basaltic samples from the Khanka Block and Sikhote-Alin accretionary complex.They are characterized by large variations in SiO_(2)contents(41 wt.%to 50 wt.%)and CaO/Al_(2)O_(3)(0.50 to 0.97),enrichments of large-ion lithophile elements(LILE),positive Nb-Ta anomalies and strongly negative K,Pb,Zr,Hf,Ti,Y anomalies in primitive mantle-normalized trace element spider diagram.Furthermore,the rocks show good correlations of Ti/Ti^(*)with Hf/Hf^(*),La/Yb,Fe/Mn and trace element contents(e.g.,Nb).In addition,they have lighter Mg and heavier Zn isotope compositions than the BSE estimates,coupled with depleted Sr-Nd isotope compositions.These elemental and isotopic characteristics cannot be explained by alteration,magma differentiation or diffusion,but are consistent with the partial melting of carbonated peridotite.By and large,the Late Mesozoic-Cenozoic basalts from far eastern Russia bear very similar geochemical characteristics as those Na-series Cenozoic basalts from eastern China.The extended region of Mg-Zn isotopic anomalies is roughly coincident with the stagnant West Pacific slab beneath East Asia,and all of these alkali basalts can be generated from mantle sources hybridized by recycled Mg-carbonates from the Pacific slab stagnant in the mantle transition zone.We infer that(1)the carbonated big mantle wedge extends to the NE edge of the West Pacific slab and may have also appeared in the Late Mesozoic due to the effect of the Paleo-Pacific slab beneath this region,and(2)decarbonation of stagnant slabs in the mantle transition zone is a key mechanism for carbon outgassing from deep mantle to surface via intraplate alkali melts.

Formation of defects in selective laser melted Inconel 718 and its correlation with mechanical properties through dimensionless numbers

This paper presents a profound study on the formation of three typical types of defects(i.e.,lack of fusion,keyholes,and gas pores)observed in selective laser melting(SLM)printed Inconel 718 samples,along with their correlations with mechanical properties of the samples.Computed tomography,scanning electron microscopy,and mechanical property tests revealed that the three types of defects fall into three stages of porosity evolution classified by recently-proposed dimensionless numbersηm(melting efficiency)andηv(vaporization efficiency).Meanwhile,experimental tests verified that the mechanical properties of products,such as strength and elongation,are remarkably sensitive to lack of fusion.However,these properties are slightly affected by the keyholes and gas pores.An optimal process window characterized by dimensionless numbers is realized by adjusting the processing parameters and employing different powders.This process window allows products to have relatively low defects and high mechanical performances.A quantitative relation between processing parameters,dimensionless numbers,defects,and mechanical properties is established based on these observations.This relation,along with the optimal process window,is believed to enhance the quality of SLM products of Inconel 718 alloy and can be further extended to SLM with other metal materials.

Learning-based phase imaging using a low-bit-depth pattern

Phase imaging always deals with the problem of phase invisibility when capturing objects with existing light sensors.However,there is a demand for multiplane full intensity measurements and iterative propagation process or reliance on reference in most conventional approaches.In this paper,we present an end-to-end compressible phase imaging method based on deep neural networks,which can implement phase estimation using only binary measurements.A thin diffuser as a preprocessor is placed in front of the image sensor to implicitly encode the incoming wavefront information into the distortion and local variation of the generated speckles.Through the trained network,the phase profile of the object can be extracted from the discrete grains distributed in the low-bit-depth pattern.Our experiments demonstrate the faithful reconstruction with reasonable quality utilizing a single binary pattern and verify the high redundancy of the information in the intensity mcasurement for phase recovery.In addition to the advantages of efficiency and simplicity compared to now available imaging methods,our model provides significant compressibility for imaging data and can therefore facilitate the low-cost detection and efficient data transmission.

Optimization of fracturing parameters for tight oil production based on genetic algorithm

It is difficult to determine the main controlling factors of tight oil production.In addition to the problem of uncontrollable prediction accuracy,the numerical prediction model established by the main controlling factors will also make the correctly predicted low production samples lose the value of development.Applying the optimization algorithm with fast convergence speed and global optimization to optimize the controllable parameters in the high-precision numerical prediction model can effectively improve the productivity of low production wells with timeliness,and bring greater economic value while saving development cost.Using PCA-GRA method,the sample weight and the weighted correlation ranking results of parameters affecting tight oil production were obtained.Thereupon then the main controlling factors of tight oil production were determined.Then we set up a BP neural network model with by taking the main controlling factors as input and tight oil production as output.The prediction effect of the network was good and can be put into use.The results of sensitivity analysis showed that the network was stable,and the total fracturing fluid volume had the greatest impact on the production of tight oil.Finally,by using genetic algorithm,we optimized the fracturing parameters of all low production well samples in the field data.Combined with the fracturing parameters of all high production well samples and the optimized fracturing parameters of low production wells,the optimal interval of fracturing parameters was given,which can provide guidance for the field fracturing operation.