Hydraulic sandblasting perforation plays a crucial role in the fracturing and reconstruction of unconventional oil and gas reservoirs.The jet nozzle is an essential part of the hydraulic perforation tool.Insufficient ...Hydraulic sandblasting perforation plays a crucial role in the fracturing and reconstruction of unconventional oil and gas reservoirs.The jet nozzle is an essential part of the hydraulic perforation tool.Insufficient penetration depth,caused by excessive jet distances,presents challenges during the perforation process.To overcome this,an optimization design of the nozzle structure is required to enhance the perforation efficiency.In this paper,a computational fluid-dynamic model for conical-cylindrical nozzles has been elaborated.To further improve the rock-breaking efficiency of the jet nozzle,a fillet design is introduced at the nozzle inlet section.The SST k-ωmodel is employed to account for turbulent flow effects in submerged conditions.The results indicate that the nozzle’s geometric parameters greatly influence the flow characteristics.The orthogonal experimental method is employed to optimize the flow channel structure of the nozzle,taking the length of constant velocity core as the evaluation index.The following optimized geometric parameters for the conical-cylindrical nozzle have been determined accordingly:a cylindrical segment diameter of 3.2 mm,a contraction angle of 12°,a contraction segment length of 8 mm,a cylindrical segment length of 6.4 mm,and a fillet radius of 2 mm.展开更多
The east-west location change of the East Asian westerly jet （EAWJ） at 200 hPa during Meiyu and the associated spatial distribution variation of precipitation in the middle-lower reaches of the Yangtze River （MLYR...The east-west location change of the East Asian westerly jet （EAWJ） at 200 hPa during Meiyu and the associated spatial distribution variation of precipitation in the middle-lower reaches of the Yangtze River （MLYR） are investigated by using the 40-yr NCEP/NCAR （National Centers for Environmental Prediction/National Center for Atmospheric Research） pentad mean reanalysis data and daily precipitation observation data from 1958 to 1997. The results show that there are two areas over which the 200-hPa EAWJ center appears most frequently during the Meiyu period： one is the western Pacific （WP） and the other is the East Asian continent （EAC）. During the Meiyu period, the westerly jet over the EAC is weak, and the core of the westerly jet over the WP splits up with reduced intensity and disappears by the end of Meiyu. The changes in the location and intensity of the westerly jet are associated not only with the starting and ending dates of Meiyu, but also with the spatial distribution and intensity of precipitation in the MLYR. It is found that when the westerly jet core in the upper troposphere is located over the WP and is coupled with an 850-hPa southwesterly jet, heavy precipitation accompanied by strong convergence and plenty supply of water vapor, occurs in the lower reaches of the Yangtze River. If the 200-hPa westerly jet core is located over the EAC, and without an 850-hPa southwesterly jet, only weak precipitation occurs in the MLYR. Therefore, the longitudinal location of the EAWJ core plays an important role in determining the upper- to lower-level circulation structure and the spatial distribution of heavy precipitation in the MLYR during the Meiyu period.展开更多
This letter reports inlet flow disturbance effects on direct numerical simulation of incompressible round jet at Reynolds number 2500.The simulation employs an accurate projection method in which a sixth order biased ...This letter reports inlet flow disturbance effects on direct numerical simulation of incompressible round jet at Reynolds number 2500.The simulation employs an accurate projection method in which a sixth order biased upwind difference scheme is used for spatial discretization of nonlinear convective terms,with a fourth order central difference scheme used in the discretization of the divergence of intermediate velocity.Carefully identifying reveals that the inlet flow disturbance has some influences on the distribution pattern of mean factor of swirling strength intermittency.With the increase of inlet disturbance magnitude jet core cone slightly shortens,observable differences occur in the centerline velocity and its fluctuations,despite the negligible impacts on the least square fitted centerline velocity decay constant(B_u)and distribution parameter(K_u)for velocity profile in self-similar region.展开更多
This paper deals with the structure of air-jet textured yarn(ATY),especilly its core structurein dedail.It is described that overfeed of supply yarn does influence the ATY structure.Then thebending rigidity of ATY has...This paper deals with the structure of air-jet textured yarn(ATY),especilly its core structurein dedail.It is described that overfeed of supply yarn does influence the ATY structure.Then thebending rigidity of ATY has been measured and analyzed.The results shows that various supplyyarns affect the core structure and bending rigidity of ATY.展开更多
利用常规观测资料、FY-2C卫星云图、NCEP/NCAR再分析资料,对一次西南低涡暴雨过程进行了诊断分析。结果表明,这次暴雨天气过程的主要影响系统有对流层高层南亚高压、中层低涡、低层切变线(低涡)以及台风"天鹅"。该过程是由3...利用常规观测资料、FY-2C卫星云图、NCEP/NCAR再分析资料,对一次西南低涡暴雨过程进行了诊断分析。结果表明,这次暴雨天气过程的主要影响系统有对流层高层南亚高压、中层低涡、低层切变线(低涡)以及台风"天鹅"。该过程是由3个接连发生的中尺度对流云团直接造成的,发生在西南低涡闭合涡旋范围内的非对称处。利用WRF_ARW(The Advanced Research WRF)中尺度模式进行了数值模拟,结果表明,对流层高层南亚高压脊线附近的强辐散、对流层中层低涡的垂直涡度耦合和对流层低层强劲的东风干冷急流与南风暖湿急流在四川盆地内交汇,促使西南低涡发展、加强。对流层高层的强辐散和低层强辐合相配合,有利于西南低涡的增强、发展。温度场上,发展的西南低涡在300hPa附近出现"暖心"结构,在850hPa以下北冷南暖,冷暖空气交界随着高度的增加向北倾斜。低涡中心南北两侧的次级环流圈上升支在低涡中心附近汇合,出现剧烈的上升运动,促使西南低涡增强。随着高层南亚高压的南移、高空急流的南压,高层辐散减弱,西南低涡也减弱。当中层西风大槽主体移过河套地区,其携带的强冷空气沿高原东侧迅速南下,大量冷空气进入四川盆地,促使西南低涡向南移出盆地,最终减弱、填塞。展开更多
基金The authors gratefully acknowledge the financial support by the National Natural Science Foundation of China(No.52405272)the CNOOC’s major project during the 14th Five-Year Plan period“Key Technologies and Equipment for Measurement,Recording,and Testing-Development and Engineering of Integrated Perforation Technology Equipment Based on Reservoir Geology”and the National Science Foundation of Jiangsu Province(No.BK20220533).
文摘Hydraulic sandblasting perforation plays a crucial role in the fracturing and reconstruction of unconventional oil and gas reservoirs.The jet nozzle is an essential part of the hydraulic perforation tool.Insufficient penetration depth,caused by excessive jet distances,presents challenges during the perforation process.To overcome this,an optimization design of the nozzle structure is required to enhance the perforation efficiency.In this paper,a computational fluid-dynamic model for conical-cylindrical nozzles has been elaborated.To further improve the rock-breaking efficiency of the jet nozzle,a fillet design is introduced at the nozzle inlet section.The SST k-ωmodel is employed to account for turbulent flow effects in submerged conditions.The results indicate that the nozzle’s geometric parameters greatly influence the flow characteristics.The orthogonal experimental method is employed to optimize the flow channel structure of the nozzle,taking the length of constant velocity core as the evaluation index.The following optimized geometric parameters for the conical-cylindrical nozzle have been determined accordingly:a cylindrical segment diameter of 3.2 mm,a contraction angle of 12°,a contraction segment length of 8 mm,a cylindrical segment length of 6.4 mm,and a fillet radius of 2 mm.
基金Supported by the National Natural Science Foundation of China under Grant No. 40675041Open Research Program of KLME, Nanjing University of Information Science & Technology
文摘The east-west location change of the East Asian westerly jet （EAWJ） at 200 hPa during Meiyu and the associated spatial distribution variation of precipitation in the middle-lower reaches of the Yangtze River （MLYR） are investigated by using the 40-yr NCEP/NCAR （National Centers for Environmental Prediction/National Center for Atmospheric Research） pentad mean reanalysis data and daily precipitation observation data from 1958 to 1997. The results show that there are two areas over which the 200-hPa EAWJ center appears most frequently during the Meiyu period： one is the western Pacific （WP） and the other is the East Asian continent （EAC）. During the Meiyu period, the westerly jet over the EAC is weak, and the core of the westerly jet over the WP splits up with reduced intensity and disappears by the end of Meiyu. The changes in the location and intensity of the westerly jet are associated not only with the starting and ending dates of Meiyu, but also with the spatial distribution and intensity of precipitation in the MLYR. It is found that when the westerly jet core in the upper troposphere is located over the WP and is coupled with an 850-hPa southwesterly jet, heavy precipitation accompanied by strong convergence and plenty supply of water vapor, occurs in the lower reaches of the Yangtze River. If the 200-hPa westerly jet core is located over the EAC, and without an 850-hPa southwesterly jet, only weak precipitation occurs in the MLYR. Therefore, the longitudinal location of the EAWJ core plays an important role in determining the upper- to lower-level circulation structure and the spatial distribution of heavy precipitation in the MLYR during the Meiyu period.
基金the financial support of the National Natural Science Foundation of China (11372303)
文摘This letter reports inlet flow disturbance effects on direct numerical simulation of incompressible round jet at Reynolds number 2500.The simulation employs an accurate projection method in which a sixth order biased upwind difference scheme is used for spatial discretization of nonlinear convective terms,with a fourth order central difference scheme used in the discretization of the divergence of intermediate velocity.Carefully identifying reveals that the inlet flow disturbance has some influences on the distribution pattern of mean factor of swirling strength intermittency.With the increase of inlet disturbance magnitude jet core cone slightly shortens,observable differences occur in the centerline velocity and its fluctuations,despite the negligible impacts on the least square fitted centerline velocity decay constant(B_u)and distribution parameter(K_u)for velocity profile in self-similar region.
文摘This paper deals with the structure of air-jet textured yarn(ATY),especilly its core structurein dedail.It is described that overfeed of supply yarn does influence the ATY structure.Then thebending rigidity of ATY has been measured and analyzed.The results shows that various supplyyarns affect the core structure and bending rigidity of ATY.
文摘利用常规观测资料、FY-2C卫星云图、NCEP/NCAR再分析资料,对一次西南低涡暴雨过程进行了诊断分析。结果表明,这次暴雨天气过程的主要影响系统有对流层高层南亚高压、中层低涡、低层切变线(低涡)以及台风"天鹅"。该过程是由3个接连发生的中尺度对流云团直接造成的,发生在西南低涡闭合涡旋范围内的非对称处。利用WRF_ARW(The Advanced Research WRF)中尺度模式进行了数值模拟,结果表明,对流层高层南亚高压脊线附近的强辐散、对流层中层低涡的垂直涡度耦合和对流层低层强劲的东风干冷急流与南风暖湿急流在四川盆地内交汇,促使西南低涡发展、加强。对流层高层的强辐散和低层强辐合相配合,有利于西南低涡的增强、发展。温度场上,发展的西南低涡在300hPa附近出现"暖心"结构,在850hPa以下北冷南暖,冷暖空气交界随着高度的增加向北倾斜。低涡中心南北两侧的次级环流圈上升支在低涡中心附近汇合,出现剧烈的上升运动,促使西南低涡增强。随着高层南亚高压的南移、高空急流的南压,高层辐散减弱,西南低涡也减弱。当中层西风大槽主体移过河套地区,其携带的强冷空气沿高原东侧迅速南下,大量冷空气进入四川盆地,促使西南低涡向南移出盆地,最终减弱、填塞。
