自然科学版
陕西师范大学学报(自然科学版)
资源与环境科学
北方典型林地系统土壤水分动态和水量平衡随机模拟研究
PDF下载 ()
李嘉1,4,5, 潘兴瑶1*, 牛勇2, 和继军3
(1 北京市水科学技术研究院, 北京 100048; 2 山东农业大学 林学院, 山东 泰安 271018;3 首都师范大学 北京市资源环境与GIS重点实验室, 北京 100048;4 河海大学 水文水资源学院, 江苏 南京 210098;5 宁夏水电技师学院, 宁夏 银川 750006)
潘兴瑶,男,高级工程师。E-mail:041087@163.com
摘要:
以我国北方干旱半干旱地区3种典型林地植被元宝枫、油松、侧柏为研究对象,基于实测数据验证和构建土壤水分动态随机模型,量化区域土壤水分随机分布、水量平衡过程及其水分胁迫特征。结果显示:模型可较好地模拟3种林地的土壤水分动态分布特征,3种林地的土壤湿度概率密度分布区间接近,呈单峰状;大部分土壤水分通过蒸散发损耗且以胁迫蒸散发为主,土壤层深层渗漏量所占比例较小且几乎不产流,符合我国北方干旱半干旱山区林地水循环的实际特征;3种林地系统均受到一定程度的水分胁迫且水分胁迫特征值相近,表明土壤水分条件是影响区域生态系统的决定性因素。
关键词:
土壤湿度概率密度函数; 水量平衡; 水分胁迫; 林地; 干旱半干旱地区
收稿日期:
2016-11-01
中图分类号:
S152.7
文献标识码:
A
文章编号:
1672-4291(2017)02-0080-08doi:10.15983/j.cnki.jsnu.2017.02.421
基金项目:
国家自然科学基金(41301019,41401302); 北京市科技计划项目(D161100005916001,D161100005916003)
Doi:
Study on probabilistic modeling of soil moisture dynamics and water balance of typical forest land in northern China
LI Jia1,4,5,PAN Xingyao1*, NIU Yong2,HE Jijun3
(1 Beijing Water Science and Technology Institute, Beijing 100048, China;2 Forestry College of Shandong Agricultural University, Tai′an 271018, Shandong, China;3 Resources Environment and GIS Key Laboratory of Beijing, Capital Normal University, Beijing 100048,China;4 College of Hydrology and Water Resources, Hohai University, Nanjing 210098, Jiangsu, China;5 Ningxia Technician College of Water Resources and Electric Power, Yinchuan 750006, Ningxia, China)
Abstract:
Using the measured data to verify and construct the stochastic model of soil moisture dynamic,three typical forest ecosystems of maple, pine and cypress forest land were selected to quantify regional soil moisture stochastic distribution, water balance process and the water stress characteristics in the arid and semi-arid area of northern China. The results showed that the stochastic model can effectively simulate the characteristics of soil moisture dynamic distribution of three typical forest land. Meanwhile, it showed the distribution range of the probability density function for three forest is similar and the curves are one-humped. Most of moisture losses from the soil is evaporation and the main part is the evapotranspiration under stressed condition.On the other hand, the soil infiltration take a very small proportion, and the runoff hardly occours which matching the real situation of the forest land in arid and semi-arid mountain areas.Three forest land is suffered a certain degree of water stress and the water stress for three forest turns out to be very similar, suggesting that soil moisture condition is the decisive factor which can influence regional ecological system.
KeyWords:
soil moisture probability density function;water balance; water stress; forest land; arid and semi-arid region