The low degree of development and utilization as well as the contradiction between supply and demand of water resources in Huangshui River basin are the main restricting factors of the local agricultural development. ...The low degree of development and utilization as well as the contradiction between supply and demand of water resources in Huangshui River basin are the main restricting factors of the local agricultural development. The study on the simulation of irrigation water loss based on the VSMB model has very important significance to strengthening regional water management and improving water resource utilization efficiency. Five groundwater wells were set up to carry out the farmland irrigation water infiltration and the experimental study on groundwater dynamic effect. Two soil moisture monitoring sites were set up in two typical plots of Daxia and Guanting irrigation area at the same time and TDR300 was used to monitor four kinds of deep soil moisture( 10 cm,30 cm,50 cm and 70 cm). On this basis,the VSMB model was used to study the irrigation water loss in the irrigation area of Yellow River valley of Qinghai Province,including soil moisture content,the actual evapotranspiration,infiltration,runoff,groundwater buried depth and so on. The results showed that the water consumption caused by soil evaporation and crop transpiration accounted for 46. 4% and 24. 1% of the total precipitation plus irrigation,respectively,and the leakage accounted for 30. 3% and 60. 6% of the total precipitation plus irrigation,respectively,from March 1,2013 to April 30,and from August 1 to September 30. The actual evaporation of the GT- TR1 and GT- TR2 sites in the whole year of 2013 was 632. 6 mm and 646. 9 mm,respectively,and the leakage accounted for 2. 6% and 1. 2% of the total precipitation plus irrigation,respectively. RMSE of the simulation results of the groundwater depth in Daxia irrigation area during the two periods was 92. 3 mm and 27. 7 mm,respectively. And RMSE of the simulation results of the water content of soil profile in the two monitoring sites of Guanting irrigation area was 2. 04% and 5. 81%,respectively,indicating that the simulation results were reliable.展开更多
The development of NCZ-1 dust-sticking agent was first intreduced in china. The speed of water absorption of dust-stick-ing agent was measured and studied on mining site and in laboratory, and then the law of water ab...The development of NCZ-1 dust-sticking agent was first intreduced in china. The speed of water absorption of dust-stick-ing agent was measured and studied on mining site and in laboratory, and then the law of water absorption of dust-sticking agent was analyzed. In addition, the mathematical model of the loss rate of dust-sticking agent was established by the application of fluid mechanics theory, and the method of determining the sprinkle parameters of dust-sticking agent was obtained. Through practical verifi-cation, it is found that the error of this mathematical model is less than 10%. So it can be used in the field.展开更多
Many landslides in reservoir areas continuously deform under cyclic water level fluctuations due to reservoir operations. In this paper,a landslide model, developed for a typical colluvial landslide in the Three Gorge...Many landslides in reservoir areas continuously deform under cyclic water level fluctuations due to reservoir operations. In this paper,a landslide model, developed for a typical colluvial landslide in the Three Gorges Reservoir area, is used to study the effect of cyclic water level fluctuations on the landslide. Five cyclic water level fluctuations were implemented in the test, and the fluctuation rate in the last two fluctuations doubled over the first three fluctuations. The pore water pressure and lateral landslide profiles were obtained during the test. A measurement of the landslide soil loss was proposed to quantitatively evaluate the influence of water level fluctuations. The test results show that the first water level rising is most negative to the landslide among the five cycles. The fourth drawdown with a higher drawdown rate caused further large landslide deformation. An increase of the water level drawdown rate is much more unfavorable to the landslide than an increase of the water level rising rate. In addition, the landslide was found to have an adaptive ability to resist subsequent water level fluctuations after undergoing large deformation during a water level fluctuation. The landslide deformation and observations in the field were found to support the test results well.展开更多
Hydrologic and water quality models are often used in assessing the response of environmental processes to human activities and climatic change. However, these models differ in terms of their complexity, requirements,...Hydrologic and water quality models are often used in assessing the response of environmental processes to human activities and climatic change. However, these models differ in terms of their complexity, requirements, underlying equations, and assumptions, and as such their performance in simulating landscape processes varies. Consequently, a key question that has to be addressed is to select the most suitable model that gives results closest to reality for an intended purpose. In this study, the performance of the basin-wide older version of SWAT is compared with that of the small watershed model APEX to assess the performance of both models at a field scale level. The new restructured version of SWAT (SWAT+) is compared with the older version to determine whether the new changes incorporated in SWAT+ have improved model performance, particularly for small watersheds. The three models were used to simulate the edge of field processes for a 6.6 ha plot located at the USDA-Agricultural Research Station near Riesel, Texas, and to predict water yield, soil, and mineral phosphorous loss from the micro watershed. Results showed that all the uncalibrated models over-predict soil and phosphorous loss in a micro watershed. Uncalibrated SWAT and SWAT+ models simulated water yield satisfactory albeit with low-performance metrics. The calibrated versions simulated water yield with indices close to optimal values. PBIAS as a performance assessment metric was determined to be overly sensitive and prone to numerical errors. SWAT+ will be helpful in the understanding of hydrological and water quality processes at micro watersheds considering that it addresses structural flaws associated with the older version, and the manually calibrated version matches the performance of both APEX and SWAT, despite the latter two undergoing rigorous automatic calibration.展开更多
通过监测田面水磷素含量和形态的动态变化来研究稻田磷素流失风险.结果表明:从环境角度、经济效益和水稻生长出发,用线性+平台施肥模型得到该地区水稻的最佳施磷量为66 kg P2O5/hm2;施磷后田面水各形态磷浓度呈现急剧下降-缓慢下降-平...通过监测田面水磷素含量和形态的动态变化来研究稻田磷素流失风险.结果表明:从环境角度、经济效益和水稻生长出发,用线性+平台施肥模型得到该地区水稻的最佳施磷量为66 kg P2O5/hm2;施磷后田面水各形态磷浓度呈现急剧下降-缓慢下降-平稳的过程,但在施磷后7天内田面水磷素浓度仍然较高,是磷素流失的高危险期;用对数模型模拟田面水中各形态磷素含量与施肥时间的关系(可溶性有机磷SOP除外),其相关系数r为0.715 1～0.963 9,在P＜0.05水平下达到极显著水平,应用模型预测常规施肥下田面水的安全排放期时为施肥后24天;除P0处理外,其余各处理中田面水磷的形态以可溶性无机磷SIP为主,随着施磷量的增加,颗粒态磷PP在田面水中的浓度呈现增大的趋势,因此,在评价田面水排放或者稻田径流对水体富营养化的贡献时,颗粒态磷PP的影响也不容忽视.展开更多
基金Supported by Study of Water Consumption Coefficient in the Irrigation Area of the Yellow River Basin in Qinghai Province(QX2012-019)
文摘The low degree of development and utilization as well as the contradiction between supply and demand of water resources in Huangshui River basin are the main restricting factors of the local agricultural development. The study on the simulation of irrigation water loss based on the VSMB model has very important significance to strengthening regional water management and improving water resource utilization efficiency. Five groundwater wells were set up to carry out the farmland irrigation water infiltration and the experimental study on groundwater dynamic effect. Two soil moisture monitoring sites were set up in two typical plots of Daxia and Guanting irrigation area at the same time and TDR300 was used to monitor four kinds of deep soil moisture( 10 cm,30 cm,50 cm and 70 cm). On this basis,the VSMB model was used to study the irrigation water loss in the irrigation area of Yellow River valley of Qinghai Province,including soil moisture content,the actual evapotranspiration,infiltration,runoff,groundwater buried depth and so on. The results showed that the water consumption caused by soil evaporation and crop transpiration accounted for 46. 4% and 24. 1% of the total precipitation plus irrigation,respectively,and the leakage accounted for 30. 3% and 60. 6% of the total precipitation plus irrigation,respectively,from March 1,2013 to April 30,and from August 1 to September 30. The actual evaporation of the GT- TR1 and GT- TR2 sites in the whole year of 2013 was 632. 6 mm and 646. 9 mm,respectively,and the leakage accounted for 2. 6% and 1. 2% of the total precipitation plus irrigation,respectively. RMSE of the simulation results of the groundwater depth in Daxia irrigation area during the two periods was 92. 3 mm and 27. 7 mm,respectively. And RMSE of the simulation results of the water content of soil profile in the two monitoring sites of Guanting irrigation area was 2. 04% and 5. 81%,respectively,indicating that the simulation results were reliable.
文摘The development of NCZ-1 dust-sticking agent was first intreduced in china. The speed of water absorption of dust-stick-ing agent was measured and studied on mining site and in laboratory, and then the law of water absorption of dust-sticking agent was analyzed. In addition, the mathematical model of the loss rate of dust-sticking agent was established by the application of fluid mechanics theory, and the method of determining the sprinkle parameters of dust-sticking agent was obtained. Through practical verifi-cation, it is found that the error of this mathematical model is less than 10%. So it can be used in the field.
基金funded by the Key Program of National Natural Science Foundation of China (41630643)the National Key Research and Development Program of China (2017YFC1501302)the Fundamental Research Funds for the Central Universities, China University of Geosciences (Wuhan) (CUGCJ1701)
文摘Many landslides in reservoir areas continuously deform under cyclic water level fluctuations due to reservoir operations. In this paper,a landslide model, developed for a typical colluvial landslide in the Three Gorges Reservoir area, is used to study the effect of cyclic water level fluctuations on the landslide. Five cyclic water level fluctuations were implemented in the test, and the fluctuation rate in the last two fluctuations doubled over the first three fluctuations. The pore water pressure and lateral landslide profiles were obtained during the test. A measurement of the landslide soil loss was proposed to quantitatively evaluate the influence of water level fluctuations. The test results show that the first water level rising is most negative to the landslide among the five cycles. The fourth drawdown with a higher drawdown rate caused further large landslide deformation. An increase of the water level drawdown rate is much more unfavorable to the landslide than an increase of the water level rising rate. In addition, the landslide was found to have an adaptive ability to resist subsequent water level fluctuations after undergoing large deformation during a water level fluctuation. The landslide deformation and observations in the field were found to support the test results well.
文摘Hydrologic and water quality models are often used in assessing the response of environmental processes to human activities and climatic change. However, these models differ in terms of their complexity, requirements, underlying equations, and assumptions, and as such their performance in simulating landscape processes varies. Consequently, a key question that has to be addressed is to select the most suitable model that gives results closest to reality for an intended purpose. In this study, the performance of the basin-wide older version of SWAT is compared with that of the small watershed model APEX to assess the performance of both models at a field scale level. The new restructured version of SWAT (SWAT+) is compared with the older version to determine whether the new changes incorporated in SWAT+ have improved model performance, particularly for small watersheds. The three models were used to simulate the edge of field processes for a 6.6 ha plot located at the USDA-Agricultural Research Station near Riesel, Texas, and to predict water yield, soil, and mineral phosphorous loss from the micro watershed. Results showed that all the uncalibrated models over-predict soil and phosphorous loss in a micro watershed. Uncalibrated SWAT and SWAT+ models simulated water yield satisfactory albeit with low-performance metrics. The calibrated versions simulated water yield with indices close to optimal values. PBIAS as a performance assessment metric was determined to be overly sensitive and prone to numerical errors. SWAT+ will be helpful in the understanding of hydrological and water quality processes at micro watersheds considering that it addresses structural flaws associated with the older version, and the manually calibrated version matches the performance of both APEX and SWAT, despite the latter two undergoing rigorous automatic calibration.
文摘通过监测田面水磷素含量和形态的动态变化来研究稻田磷素流失风险.结果表明:从环境角度、经济效益和水稻生长出发,用线性+平台施肥模型得到该地区水稻的最佳施磷量为66 kg P2O5/hm2;施磷后田面水各形态磷浓度呈现急剧下降-缓慢下降-平稳的过程,但在施磷后7天内田面水磷素浓度仍然较高,是磷素流失的高危险期;用对数模型模拟田面水中各形态磷素含量与施肥时间的关系(可溶性有机磷SOP除外),其相关系数r为0.715 1～0.963 9,在P＜0.05水平下达到极显著水平,应用模型预测常规施肥下田面水的安全排放期时为施肥后24天;除P0处理外,其余各处理中田面水磷的形态以可溶性无机磷SIP为主,随着施磷量的增加,颗粒态磷PP在田面水中的浓度呈现增大的趋势,因此,在评价田面水排放或者稻田径流对水体富营养化的贡献时,颗粒态磷PP的影响也不容忽视.
