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不同雨强下黄土裸坡水-沙-氮磷流失耦合模拟
引用本文:彭梦玲,吴磊,乔闪闪. 不同雨强下黄土裸坡水-沙-氮磷流失耦合模拟[J]. 中国环境科学, 2018, 38(3): 1109-1116
作者姓名:彭梦玲  吴磊  乔闪闪
作者单位:1. 西北农林科技大学水利与建筑工程学院, 陕西 杨凌 712100;2. 西北农林科技大学, 黄土高原土壤侵蚀与旱地农业国家重点实验室, 陕西 杨凌 712100;3. 西北农林科技大学, 旱区农业水土工程教育部重点实验室, 陕西 杨凌 712100
基金项目:国家自然科学基金资助项目(51679206);陕西省青年科技新星项目(2017KJXX-91);“仲英青年学者”项目(Z111021720).
摘    要:采用室内人工模拟降雨试验研究6种雨强3种坡度下黄土裸露坡面水沙及氮磷养分流失规律.结果表明:1)降雨强度与土壤入渗速率,坡面产流产沙量的线性拟合决定系数均大于0.8,有较好的正相关关系;2)25°黄土坡面下:NO3--N初始浓度较高,随降雨历时呈波动性减少,具有明显的初期冲刷效应;NH4+-N初始流失浓度由90mm/h雨强下0.6057mg/L增至120mm/h的1.3076mg/L,但其浓度随降雨历时均不断减小;TN流失浓度在雨强为90,105和120mm/h时分别为0.6056,0.8011和1.3076mg/L,随雨强增大而增大;TP初始流失浓度在105mm/h时最大,90mm/h时最小,且不同雨强下TP流失浓度相互交错,不稳定;3)养分流失与坡面产流量具有较强的线性相关性,与产沙量呈显著的幂函数关系.15°坡面时,氮素流失在6种雨强下均以颗粒态为主,平均约占72%,但在雨强增大过程中,颗粒态所占比例先减少后增加;而磷素流失颗粒态所占比例均大于90%,与降雨强度和坡度均没有直接关系.

关 键 词:雨强  黄土坡面  裸地  产流产沙  氮磷流失  
收稿时间:2017-08-15

Coupling simulation of runoff-sediment-nutrient loss on loess bare sloping land under different rainfall intensities
PENG Meng-ling,WU Lei,QIAO Shan-shan. Coupling simulation of runoff-sediment-nutrient loss on loess bare sloping land under different rainfall intensities[J]. China Environmental Science, 2018, 38(3): 1109-1116
Authors:PENG Meng-ling  WU Lei  QIAO Shan-shan
Affiliation:1. College of Water Resources and Architectural Engineering, Northwest A & F University, Yangling 712100, China;2. State Key Laboratory of Soil Erosion and Dryland Farming on the Loess Plateau, Institute of Water and Soil Conservation, Northwest A & F University, Yangling 712100, China;3. Key Laboratory of Agricultural Soil and Water Engineering in Arid and Semiarid Areas, Ministry of Education, Northwest A & F University, Yangling 712100, China
Abstract:The simulated rainfall experiment was conducted to explore the effect of rainfall intensity on coupling loss rules of runoff and sediment and nutrients under different loess bare slopes.Results showed that:1) The linear fitting coefficients between rainfall intensity and soil infiltration rate,runoff or sediment were all greater than 0.8,there were strong positive correlations;2) At 25°slope:The initial NO3--N concentration was high,it was decreased with increased rainfall duration,the scouring effect was significant;The initial NH4+-N concentration increased from 0.6057 to 1.3076mg/L with increased rainfall intensity from 90 to 120mm/h,but NH4+-N concentration decreased with increased rainfall duration;TN concentrations were 0.6056,0.8011 and 1.3076mg/L under rainfall intensities of 90,105 and 120mm/h,which increased with increased rainfall intensity;The initial TP concentration had the maximum value in 105mm/h and the minimum value in 90mm/h,and TP concentrations in different rainfall intensities were intertwined and unstable.3) There was a strong linear correlation between runoff yield and nutrient loss,while there was a significant power correlation between sediment and nutrient loss.At 15°slope:the loss forms of nitrogen was mainly in particulate state under six rainfall intensities,which approximately accounted for an average of 72%,but the proportion of particulate nitrogen decreased first and then increased with increased rainfall intensity;the contribution of particulate phosphorus accounted for more than 90%,which was no direct relation with rainfall intensity and slope.
Keywords:rainfall intensities  loess slope  bare land  runoff and sediment  loss of nitrogen and phosphorus  
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