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我们在土壤水动态模拟模型方面的研究工作——主要论文汇总
热度 2 shangsh 2012-11-9 21:16
今天“土壤水研究”群组获批开张,总结一下我们在 过去 10余 年中开展的土壤水分动态模型模型研究工作,与各位群友交流。也特别邀请同行加入土壤水研究群组( http://bbs.sciencenet.cn/forum.php?mod=groupfid=620 ),共同探讨土壤水问题,交流研究心得与成果。 1. 指数消退模型: (1) 简单指数模型:尚松浩,雷志栋,杨诗秀 . 冬小麦田间墒情预报的经验模型.农业工程学报, 2000 , 16(5): 31 – 33. ( http://www.tcsae.org/ch/reader/view_abstract.aspx?flag=1file_no=20000508journal_id=nygcxb ) (2) 扩展指数模型: Shang Songhao, Mao Xiaomin. A physicoempirical model for soil water simulation in crop root zone. Pedosphere, 2011, 21(4): 512 – 521. ( http://blog.sciencenet.cn/home.php?mod=attachmentid=7364 ) (3) 模拟农田土壤水分动态的二参数指数消退模型 (2014.3.14 on line ): Shang Songhao, Mao Xiaomin. A two-parameter exponential recession model for simulating cropland soil moisture dynamics. Chinese Geographical Science , 2014. doi: 10.1007/s11769-014-0676-3. http://link.springer.com/article/10.1007/s11769-014-0676-3?sa_campaign=email/event/articleAuthor/onlineFirst 2. 人工神经网络模型:尚松浩,毛晓敏,雷志栋,杨诗秀.冬小麦田间墒情预报的 BP 神经网络模型.水利学报, 2002 , (4): 60 – 63. ( http://jhe.ches.org.cn/jhe/ch/reader/view_abstract.aspx?flag=1file_no=020412journal_id=jhe ) 3. 水量平衡模型及其应用: Shang Songhao, Mao Xiaomin. Application of a simulation based optimization model for winter wheat irrigation scheduling in North China. Agricultural Water Management, 2006, 85(3): 314 – 322. ( http://dx.doi.org/10.1016/j.agwat.2006.05.015 ) 下载: 200610AGWAT_Application of a simulation based optimization model for winter whea.pdf 4. 冻土水热耦合模型及其应用: (1) 冻土水热耦合迁移模型:尚松浩,雷志栋,杨诗秀.冻结条件下水热耦合迁移数值模拟的改进.清华大学学报, 1997 , 37(8): 62 – 64 ( 下载: 1997qhdxxb冻结条件下土壤水热耦合迁移数值模拟的改进.pdf ) (2) 模型应用 1 ——土壤冻结过程中潜水蒸发:雷志栋,尚松浩,杨诗秀,王 义,赵冬梅.土壤冻结过程中潜水蒸发规律的模拟研究.水利学报, 1999 , (6): 6 – 10. ( http://jhe.ches.org.cn/jhe/ch/reader/view_abstract.aspx?flag=1file_no=990602ljournal_id=jhe ) (3) 模型应用 2 ——土壤冻融过程中地下水位变化:尚松浩,雷志栋,杨诗秀,王 义,赵冬梅.冻融期地下水位变化情况下土壤水分运动的初步研究.农业工程学报, 1999 , 15(2): 64 – 68. ( http://www.tcsae.org/ch/reader/view_abstract.aspx?flag=1file_no=19990214journal_id=nygcxb ) (4) 冻土—大气系统水热传输模型:尚松浩,雷志栋,杨诗秀.冬灌对越冬期土壤水分状况影响的数值模拟.农业工程学报, 1997 , 13(3): 65 – 70. ( http://www.tcsae.org/ch/reader/view_abstract.aspx?flag=1file_no=19970313journal_id=nygcxb ) 5. 土壤—植物—大气连续体( SPAC )水分传输模型: Shang Songhao, Li Xichun , Mao Xiaomin, Lei Zhidong . Simulation of water dynamics and irrigation scheduling for winter wheat and maize in seasonal frost areas . Agricultural Water Management , 2004 , 68(2): 117 – 133. ( http://dx.doi.org/10.1016/j.agwat.2004.03.009 ) 下载: 200610AGWAT_Application of a simulation based optimization model for winter whea.pdf 6. SPAC 水热耦合传输模型: Yang Yuting, Shang Songhao, Guan Huade. Development of a soil-plant-atmosphere continuum model (HDS-SPAC) based on hybrid dual-source approach and its verification in wheat field. Science China Technological Sciences, 2012, 55(10): 2671 – 2685. DOI: 10.1007/s11431-012-4974-7. ( http://tech.scichina.com:8082/sciEe/EN/abstract/abstract508574.shtml ) ( 2009 年以前的相关研究工作已汇集在:尚松浩,毛晓敏,雷志栋,杨诗秀. 土壤水分动态模拟模型及其应用. 科学出版社, 2009 . http://bbs.sciencenet.cn/blog-39095-241519.html )
个人分类: 论著|6188 次阅读|7 个评论
基于混合双源模式的土壤-植物-大气连续体模型及其在小麦田的检验
shangsh 2012-8-9 08:40
SCIENCE CHINA Technological Sciences 2012, DOI: 10.1007/s11431-012-4974-7 Development of a soil-plant-atmosphere continuum model (HDS-SPAC) based on hybrid dual-source approach and its verification in wheat field 摘要及全文下载 : 201210-SC-TS-Development of a soil-plant-atmosphere continuum model (HDS-SPAC) b.pdf http://tech.scichina.com:8082/sciEe/EN/abstract/abstract508574.shtml YuTing Yang , SongHao Shang and Huade Guan Abstract HDS-SPAC, a new soil-plant-atmosphere continuum (SPAC) model, is developed for simulating water and heat transfer in SPAC. The model adopts a recently proposed hybrid dual source approach for soil evaporation and plant transpiration partitioning. For the above-ground part, a layer approach is used to partition available energy and calculate aerodynamic resistances, while a patch approach is used to derive sensible heat and latent heat fluxes from the two sources (soil and vegetation). For the below-ground part, soil water and heat dynamics are described by the mixed form of Richards equation, and the soil heat conductivity equation, respectively. These two parts are coupled through ground heat flux for energy transfer, root-zone water potential-dependent stomatal resistance, and surface soil water potential-dependent evaporation for water transfer. Evaporation is calculated from the water potential gradient at soil-atmosphere interface and aerodynamic resistance, and transpiration is determined using a Jarvis-type function linking soil water availability and atmospheric conditions. Some other processes, such as canopy interception and deep percolation, are also considered in the HDS-SPAC model. The hybrid dual-source approach allows HDS-SPAC to simulate heat and water transfer in an ecosystem with a large range of vegetation cover change temporally or spatially. The model was tested with observations at a wheat field in North China Plain over a time of three months covering both wet and dry conditions. The fractional crop covers change from 30% to over 90%. The results indicated that the HDS-SPAC model can estimate actual evaporation and transpiration partitioning and soil water content and temperature over the whole range of tested vegetation coverage.
个人分类: 论著|4451 次阅读|0 个评论

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