研究兴趣
1. 有机-矿物相互作用；
2. 矿物表面物理化学行为；
3. 有机质赋存及生烃机理；
4. 页岩油气赋存与成藏机理；
5. 油气资源评价
科研项目
2016-2020，国家油气重大专项，济阳坳陷古近系烃源岩有机-无机协同演化及其资源潜力评价，参与。
2016-2019，国家油气重大专项，长江坳陷油气资源潜力评价，参与。
2016-2018，博士后科学基金，泥页岩中不同可动性有机质的相继分离及赋存特征研究，负责。
2014-2017，国家自然科学基金，泥页岩中不同赋存态烃的分离及特征研究，参与。
研究成果
[1] Zhu, X.J.*, Cai, J.G., Wang, G.L., Ji, J.F., 2020. The influence of organic matter on mineral surface area measurement of mudrocks by ethylene glycol monoethyl ether adsorption. Applied Clay Science 193, 105666.
[2] Zhu, X.J.*, Cai, J.G., Wang, Y.S., Liu, H.M., Zhang, S.P., 2020. Evolution of organic-mineral interactions and implications for organic carbon occurrence and transformation in shale. GSA Bulletin 132, 784-792.
[3] Cai, J.G.*, Zhu, X.J. (co-first author), Zhang, J.Q., Song, M.S., Wang, Y.S., 2020. Heterogeneities of organic matter and its occurrence forms in mudrocks: Evidence from comparisons of palynofacies. Marine and Petroleum Geology 111, 21-32.
[4] Zhu, X.J.*, Cai, J.G.*, Liu, Q., Li, Z., Zhang, X.J., 2019. Thresholds of petroleum content and pore diameter for petroleum mobility in shale. AAPG Bulletin 103, 605-617.
[5] Zhu, X.J.*, Cai, J.G.*, Wang, G.L., Song, M.S., 2018. Role of organo-clay composites in hydrocarbon generation of shale. International Journal of Coal Geology 192, 83-90.
[6] Zhu, X.J., Cai, J.G.*, Liu, W.X., Lu, X.C., 2016. Occurrence of stable and mobile organic matter in the clay-sized fraction of shale: Significance for petroleum geology and carbon cycle. International Journal of Coal Geology 160, 1-10.
[7] Zhu, X.J.*, Cai, J.G., 2015. Influence and Significance of Mineral Surface on Organic Matter Occurrence in Shale. Acta Geologica Sinica (English Edition) 87(supp.), 180-181.
[8] Zhu, X.J.,Cai, J.G.*,Song, G.Q., Ji, J.F., 2015.Factors influencing the specific surface areas in argillaceous source rocks. Applied Clay Science 109, 83-94.
[9] Zhu, X.J., Cai, J.G.*, Wang, X.J., Zhang, J.Q., Xu, J.L., 2014. Effects of organic components on the relationships between specific surface areas and organic matter in mudrocks.International Journal of Coal Geology 133, 24-34.
[10] Zhu, X.J., Cai, J.G.*, Xu, X.Y., Xie, Z.H., 2013. Discussion on the method for determining BET specific surface area in argillaceous source rocks. Marine and Petroleum Geology 48, 124-129.
[11] 朱晓军*, 蔡进功, 徐蒙, 刘惠民, 谢忠怀, 李政, 2017. 沾化凹陷沙三下亚段成熟泥页岩纳米孔隙体积影响因素分析及意义. 高校地质学报23, 697-705.
[12] 朱晓军, 蔡进功, 2012. 泥质烃源岩比表面与有机质关系及其意义. 石油与天然气地质 33, 375-384.
参与发表论文
[13]Li, X., Cai, J.G.*, Liu, H.M., Zhu, X.J., Li, Z., Liu, J., 2020. Characterization of shale pore structure by successive pretreatments and its significance. Fuel 269, 117412.
[14] Cai, J.G.*, Du, J.Z., Chen, Z.W., Lei, T.Z., Zhu, X.J., 2018.Hydrothermal experiments reveal the influence of organic matter on smectite illitization.Clays and Clay Minerals 66, 28-42.
[15] 袁灵聪, 朱晓军, 蔡进功*, 钟锴, 2020. 东海盆地长江坳陷美人峰组烃源岩沉积环境与生烃潜力评价. 沉积学报, 待刊.
[16] 刘伟新*, 朱晓军, 马安林, 蔡进功, 卢龙飞, 2016. 不同泥岩相有机质赋存特征及对比表面积的影响——以沾化凹陷古近系为例. 石油实验地质38, 1-7.
教学情况
主讲课程：
《常规与非常规地质学》（博士生，承担部分）