春、秋季台湾海峡海-气CO2通量及其影响因素

于2014年的5月（春季）和9月（秋季）在台湾海峡及其邻近南海和东海海域,采用水气平衡法进行了2个航次的海表和大气pCO2连续走航观测,同时获取了海表温度、海表盐度、风速及气压等数据,并采用海-气CO2分压差减法估算了海-气CO2通量.结果显示,春、秋2个航次平均海表pCO2分别为387±16μatm和408±18μatm.温度是影响台湾海峡及其邻近海域海表pCO2的主控因子,水团混合和其他因素等也对海表pCO2有一定影响.2014年春、秋季节,对研究区域的海-气CO2释放通量的估算结果分别为0.11±1.60 mmol/（m2·d）和2.51±1.10 mmol/（m2·d）.台湾海峡海表pCO2既存在显著的季节变化,又存在较大的空间差异.国家海洋局第三海洋研究所基本科研业务费资助项目(海三科2011015);;厦门南方海洋研究中心资助项目(14GHS016NF16,14PST63NF27

油井清、防蜡技术研究现状

主要介绍了目前常用的机械清防蜡、热力清防蜡、表面能防蜡 (内衬和涂料油管 )、化学剂清防蜡、超声波清防蜡、强磁清防蜡和微生物清防蜡技术等。生产实践中 ,应根据油井的含水、含蜡量选用合适的清防蜡技术 ,才能对清防蜡达到经济、满意的效果

Effects of PAA on Soil Preserving Water and Evaporation

采用土柱法研究了不同PAA施入量对3种黄土高原主要土壤类型(黄绵土、黑垆土和塿土)的持水性能、土壤饱和导水率和土壤蒸发量的影响,以进一步阐明PAA的保水和蒸发作用。结果表明,施入PAA提高了土壤的持水性能。在未加入PAA之前黑垆土的持水性能最低,塿土的最高,黄绵土的次之;加入PAA后,黑垆土的持水能力显著增加,几乎为对照的2倍,塿土和黄绵土也都比对照高。土壤的供水能力随PAA用量的增加而增强,不同土壤类型之间表现为:塿土>黑垆土>黄绵土。未加入PAA时,3种土壤饱和导水率大小为:塿土>黑垆土>黄绵土;加入PAA后,3种土壤的饱和导水率都降低,且基本随PAA用量的增加而降低。在一定水分条件下,PAA的施入提高了土壤的抗蒸发性能,随PAA用量的增加,塿土和黑垆土的土壤蒸发量增加,但都低于对照,而黄绵土的土壤蒸发量随PAA用量的增加而降低。其中施PAA54.5 mg/kg的塿土、黑垆土和施PAA225.8 mg/kg的黄绵土与对照相比,土壤蒸发量分别减少了44.0%,44.6%和30.6%

含裂缝岩石油水两相渗流的有限元模拟

利用具备自主产权的国产有限元程序自动生成系统(FEPG),模拟岩心尺度下裂缝-基质双重介质中油水两相渗流，分析压缩系数、非均质性以及注水方式对两相渗流的影响，并在此基础上考虑裂缝形态及分布方式，得出裂缝对水驱油的影响规律。结果表明：平行于主渗流方向的裂缝会导致见水时间缩短，水相沿裂缝窜流，降低驱油效果；裂缝位于双重介质内部时，基质中油相先向裂缝流动，随后缓慢排出，最终裂缝及其周围基质孔隙中的油大部分残余；垂直于主渗流方向的裂缝能有效延长见水时间，提高基质动用率。压缩系数小、非均质性弱的储层更适宜采用注水的开采方式；脉冲注水能有效提高驱油效率，加快油水界面推进速度，且频率越高效果越显著

Measurement of integrated luminosity of data collected at 3.773 GeV by BESIII from 2021 to 2024

We present a measurement of the integrated luminosity e+e- of collision data collected by the BESIII detector at the BEPCII collider at a center-of-mass energy of Ecm = 3.773 GeV. The integrated luminosities of the datasets taken from December 2021 to June 2022, from November 2022 to June 2023, and from October 2023 to February 2024 were determined to be 4.995±0.019 fb-1, 8.157±0.031 fb-1, and 4.191±0.016 fb-1, respectively, by analyzing large angle Bhabha scattering events. The uncertainties are dominated by systematic effects, and the statistical uncertainties are negligible. Our results provide essential input for future analyses and precision measurements

Determination of the number of ψ(3686) events taken at BESIII

The number of ψ(3686) events collected by the BESIII detector during the 2021 run period is determined to be (2259.3±11.1)×106 by counting inclusive ψ(3686) hadronic events. The uncertainty is systematic and the statistical uncertainty is negligible. Meanwhile, the numbers of ψ(3686) events collected during the 2009 and 2012 run periods are updated to be (107.7±0.6)×106 and (345.4±2.6)×106, respectively. Both numbers are consistent with the previous measurements within one standard deviation. The total number of ψ(3686) events in the three data samples is (2712.4±14.3)×10^