[1]Sun S J, Meng P, Zhang J S,et al,.2014. Partitioning oak woodland evapotranspiration in the rocky mountainous area of North China was disturbed by foreign vapor, as estimated based on non-steady-state 18O isotopic composition.Agricultural and Forest Meteorology, 184: 36-47
[2]Tong Xiaojuan, Zhang Jinsong*, Meng, Ping, ,et al,. 2014. Ecosystem water use efficiency in a warm-temperate mixed plantation in the North China. Journal of Hydrology 512(6): 221-228
[3]XiaojuanTong, PingMeng, JinsongZhang, et al,. 2012. Ecosystem carbon exchange over a warm-temperate mixed plantation in the lithoid hilly area of the North China.Atmospheric Environment, 49:257e267
[4]Huan hui, Zhang Jinsong, Meng Ping,et al,.2011. Seasonal Variation and Meteorological Control of CO2 Flux in a Hilly Plantation in the Mountain Areas of North China. Acta Meteorologica Sinica , (2): 238-248.
[5]郑宁,孟平, 张劲松,等.2013.闪烁仪法测算丘陵山地人工林显热通量的参数敏感性分析.林业科学研究, 26(2): 140-144
[6]郑宁, 陆森,张劲松,等.2013.华北南部低丘山地刺槐林土壤温度与冠层气温关系的研究.林业科学研究,26(1): 107-112
[7]郑宁,孟平,张劲松,等.2012.LAS测算森林冠层上方温度结构参数的可行性. 生态学报,32(7):2166-2173
[8]王平 张劲松 孟平,等.2011.华北低丘山地栓皮栎人工林土壤呼吸变化特征及其与撂荒地的差异.中国农业气象, 32( 3) 346-349
[9]同小娟, 张劲松, 孟平,等.2010.华北低丘山地人工混交林净生态系统碳交换的变化特征.林业科学, 46(3): 37-43
[10]张劲松,孟平,郑宁,等.2010.大孔径闪烁仪法测算低丘山地人工混交林显热通量的可行性分析. 地球科学进展,25(11):1283-1290
[11]国琳 张劲松, 孟平,等.2010.山茱萸光合及水分利用特征对土壤水分胁迫的响应.河北农业大学学报, 33(1): 21-26
[12]郑宁,张劲松, 孟平,等.2010.基于闪烁仪观测低丘山地人工混交林通量印痕与源区分布,地球科学进展, 25(11): 1175-1186
[13]桑玉强, 郭芳, 张劲松,等2009.毛乌素沙地新疆杨蒸腾变化规律及其影响因素.林业科学,45(9): 66-71
[14]同小娟,张劲松,孟平,等2009.华北低丘山地人工林生态系统净碳交换与气象因子的关系.生态学报, 29(12): 6638-6645
[15]张劲松, 孟平, 高峻,等2009.杜仲人工林蒸腾时间演变的分形特征及可预报时长. 林业科学研究, 22(6): 807-812