[1] Li N, Long JH, Han XZ, Yuan YR, Sheng M. Molecular characterization of soil organic carbon in water-stable aggregate fractions during the early pedogenesis from parent material of Mollisols. Journal of Soils and Sediments. 2020, 20,1869-1880.
[2] Sheng M, Han XZ, Zhang YH, Long JH, Li N*. 31-year contrasting agricultural managements affect the distribution of organic carbon in aggregate-sized fractions of a Mollisol. Scientific Reports. 2020, 10, 9041.
[3] Li N, You MY, Zhang B, Han XZ, Panakoulia SK, Yuan YR, Liu K, Qiao YF, Zou WX, Nikolaidis NP, Banwart SA. Modeling soil aggregation at the early pedogenesis stage from the parent material of a Mollisol under different agricultural practices. Advances in Agronomy. 2017, 142, 181-214.
[4] Li N, Pan FJ, Han XZ, Zhang B. Development of soil food web of microbes and nematodes under different agricultural practices during the early stage of pedogenesis of a Mollisol. Soil Biology & Biochemistry. 2016, 98, 208-216.
[5] Li N, Yao SH, Qiao YF, Zou WX, You MY, Han XZ, Zhang B. Separation of soil microbial community structure by aggregate size to a large extent under agricultural practices during early pedogenesis of a Mollisol. Applied Soil Ecology. 2015, 88, 9-20.
[6] Li N, Xu YZ, Han XZ, He HB, Zhang XD, Zhang B. Fungi contribute more than bacteria to soil organic matter through necromass accumulation under different agricultural practices during the early pedogenesis of a Mollisol. European Journal of Soil Biology. 2015, 67, 51-58.
[7] Li N, Yao SH, You MY, Zhang YL, Qiao YF, Zou WX, Han XZ, Zhang B. Contrasting development of soil microbial community structure under no-tilled perennial and tilled cropping during early pedogenesis of a Mollisol. Soil Biology & Biochemistry. 2014, 77, 221-232.
[8] Li N, Wang GX, Liu GS, Lin Y, Sun XY. The ecological implications of land use change in the Source Regions of the Yangtze and Yellow Rivers, China. Regional Environmental Change. 2013, 13, 1099-1108.
[9] Li N, Wang GX, Yang Y, Gao YH, Liu GS. Plant production, and carbon and nitrogen source pools are strongly intensified by experimental warming in alpine ecosystems in the Qinghai-Tibet Plateau. Soil Biology & Biochemistry, 2011, 43, 942-953.
[10]李娜, 韩晓增, 盛明, 龙静泓. 东北黑土成土母质培肥过程中土壤肥力变化特征. 应用生态学报, 2020, 31(4), 1155-1162
[11]盛明, 龙静泓, 雷琬莹, 郝翔翔, 李娜*, 韩晓增, 李禄军. 秸秆还田对黑土团聚体内有机碳红外光谱特征的影响. 土壤与作物, 2020, 9(4), 353-366
[12]苑亚茹, 韩晓增, 李娜*, 尤孟阳, 邹文秀. 不同熟化措施对黑土母质发育的新成土壤有机碳库的影响. 生态学杂志, 2020, 39(4), 1175-1182
[13]李娜, 张一鹤, 韩晓增, 尤孟阳, 郝翔翔. 长期不同植被覆盖对黑土团聚体内有机碳组分的影响. 植物生态学报, 2019, 43 (7), 624-634.
[14]盛明, 韩晓增, 龙静泓, 李娜*. 中国不同地区土壤有机质特征比较研究. 土壤与作物, 2019, 8(3), 320-330.
[15]李娜, 盛明, 韩晓增, 尤孟阳. 应用13C核磁共振技术研究土壤有机质化学结构进展. 土壤学报, 2019, 56(4), 810-826.
[16]李娜, 张一鹤, 韩晓增, 尤孟阳, 郝翔翔. 长期不同植被覆盖对黑土团聚体内有机碳组分的影响. 植物生态学报, 2019, 43 (7), 624-634
[17]李娜, 韩晓增, 尤孟阳, 许玉芝. 土壤团聚体与微生物相互作用研究. 生态环境学报. 2013, 22(9), 1625-1632.