Three types of natural soils are studied in this paper: 1) a postglacial silt, 2) a glacial till, and 3) a postglacial sand. The former two are soils from embankment dam sites in Sweden, and the latter is a soil from ...Three types of natural soils are studied in this paper: 1) a postglacial silt, 2) a glacial till, and 3) a postglacial sand. The former two are soils from embankment dam sites in Sweden, and the latter is a soil from a natural deposit situated in the Swedish east coastal region. In situ Double-ring infiltrometer (DRI) tests are compared with laboratory constant-head permeability determinations. This study shows that the DRI tests conducted on sandy-silty soils are within sufficient range to the laboratory results, to suggest that in situ near-saturated infiltration capacity may be used as a field estimate of hydraulic conductivity (permeability) for this range of soils. In situ infiltrometer testing may be the better alternative when there is difficulty in achieving representative field conditions in a laboratory setting, e.g., for widely graded soils such as glacial tills.展开更多
Different land use,and associated variations in agricultural or silvicultural practices,can cause substantial variations in soils’hydraulic properties.Thus,the optimal method for measuring these properties may vary,e...Different land use,and associated variations in agricultural or silvicultural practices,can cause substantial variations in soils’hydraulic properties.Thus,the optimal method for measuring these properties may vary,even among neighboring sites.In this study these variations were examined by comparing measurements of hydraulic properties of soil in fields used for poplar,alfalfa and wheat cultivation obtained with two steady flow methods(the White and Sully,and single disc with multiple tension methods)and two transient flow methods(the single disc with single tension,and multiple tensions with multiple disc radius methods).The fields were all located in Changwu municipality,a major grain-producing area in Shaanxi Province,China.Disc tension infiltrometers were used to measure unconfined,unsaturated infiltration over a range of supply pressure heads(h=−9 cm,−6 cm,−3 cm and 0)at the soil surface.Intact soil cores were sampled near the surface to determine bulk density and soil water retention curves at potentials ranging from−0.15 kPa to−100 kPa.Unsaturated hydraulic conductivity values over the range of supply pressure heads were estimated using Wooding’s equation for steady-state flow from a disc source.The van Genuchten water retention model was fitted to experimental data to estimate the parameter values.The results indicated that land use affects soils’saturated and unsaturated hydraulic conductivity.Further,steady state flow methods are most appropriate for measuring hydraulic properties of soils under poplar and wheat,due to their high organic contents and saturated hydraulic conductivity.However,for soils supporting alfalfa(which are more homogeneous),instant methods provide better results,in addition to substantial time and labor savings.展开更多
A simple method was developed to relate soil sorptivity to hydraulic diffusivity and water absorption experiments were conducted utilizing one-dimensional horizontal soil columns to validate the relationship. In addit...A simple method was developed to relate soil sorptivity to hydraulic diffusivity and water absorption experiments were conducted utilizing one-dimensional horizontal soil columns to validate the relationship. In addition, an estimation method for hydraulic diffusivity with disc infiltrometer was developed. The results indicated a favorable fit of the theoretical relation to the experimental data. Also, the experiment with disc infiltrometer for estimating the diffusivity showed that the new method was feasible.展开更多
A high degree of uncertainty with regard to soil parameterisation limits the significance of physically-based simulation of distributed flood control measures, which affect the runoff generation process, such as land-...A high degree of uncertainty with regard to soil parameterisation limits the significance of physically-based simulation of distributed flood control measures, which affect the runoff generation process, such as land-use changes or differing soil tillage practices. In this study, the soil measurement data from the hillslope scale at the Scheyern research farm were compared to demonstrate this uncertainty. To account for the spatial variability of soils in the investigation area of Scheyern, different approaches were applied to estimate soil hydraulic properties and saturated hydraulic conductivity, and were compared to field measurements展开更多
Soil formation is often a very slow process that requires thousands and even millions of years. Human influence, occasionally on a par with the function of climate or geological forces, can accelerate the process and ...Soil formation is often a very slow process that requires thousands and even millions of years. Human influence, occasionally on a par with the function of climate or geological forces, can accelerate the process and can be viewed as a distinct soil forming factor. This paper describes a soil, Haplic Regosol, in which anthrosolization dominates the soil forming process. Man-made soils, Technosols, were stabilized with techniques of ecological engineering (crib walls). We measured the main soil properties and focused on the movement of water (the reduction of soil weight is the key factor in stabilizing these calcschists). The newly deposited debris, sheltered by anthropic interventions, after four years differentiated an A/C profile while after forty years differentiated an O/A/AB/Bw/BC/C profile. Our results indicate that colonization by plants and the consequent success of vegetation establishment is influenced mainly by control of the factor of pedogenesis 'topography' and by the ability of these Technosols to retain nutrients.展开更多
An infiltration characteristic model was developed by using the modified Kostiakov method for the Agricultural Engineering demonstration field of Bangladesh Agricultural Research Institute (BARI). The constant values ...An infiltration characteristic model was developed by using the modified Kostiakov method for the Agricultural Engineering demonstration field of Bangladesh Agricultural Research Institute (BARI). The constant values a, α, and b of the equation for accumulated infiltration y = atα + b were 9.12, 0.683, and 0.145, respectively. The average value of percentage of error between the actual and calculated values by the model was only 0.134 and showed very good agreement between the model and the field values of accumulated infiltration. This model will be very helpful for making a good irrigation scheduling and best water management.展开更多
Infiltration is an important component of the hydrological cycle. It provides soil moisture in the vadose zone to support plant growth. This study was conducted to compare the validity of four infiltration models with...Infiltration is an important component of the hydrological cycle. It provides soil moisture in the vadose zone to support plant growth. This study was conducted to compare the validity of four infiltration models with measured values from the double ring infiltrometer. The parameters of the four models compared were estimated using the linear regression analysis. The C.C was used to show the performance of the predictability of the models. The RMSE, MAE and MBE were employed to check the anomalies between the predicted and the observed values. The results showed that, average values of the C.C ranged from 0.9294 - 0.9852. The average values of the RMSE were 4.0033, −17.489, 11.2400 and 49.8448;MAE were 3.1341, 15.9802, 10.6525, and 61.4736;and MBE were 0.0786, 9.5755, 0.0007 and 47.0204 for Philip, Horton, Green Ampt and Kostiakov respectively for the wetland soils. Statistical results also from the Fisher’s multiple comparison test show that the mean infiltration rate estimated from the Green Ampt’s, Philip’s and Horton’s model was not significantly different (p > 0.05) from the observed. The results indicated that the Kostiakov’s model had the highest deviations as it overestimated the measured data in all the plots. Comparison of the statistical parameters C.C, RMSE, MAE, and MBE for the four models indicates that the Philip’s model agreed well with the measured data and therefore, performed better than the Green Ampt’s, Horton’s and Kostiakov’s models respectively in that order for Besease wetland soils. Estimation of infiltration rate by the Philip’s model is important in the design of irrigation schemes and scheduling. Therefore, in the absence of measured infiltration data, the Philip’s model could be used to produce infiltration information for inland valley bottom soils that exhibit similar characteristic as Besease wetland soils.展开更多
Infiltration is an important part of the hydrological cycle, and it is one of the main abstractions accounted for in the rainfall-runoff modeling. The main purpose of this study is to compare the infiltration models t...Infiltration is an important part of the hydrological cycle, and it is one of the main abstractions accounted for in the rainfall-runoff modeling. The main purpose of this study is to compare the infiltration models that were used to assess the infiltration rate of the Mitidja Plain in Algeria. Field infiltration tests were conducted at 40 different sites using a double ring infiltrometer. Five statistical comparison criteria including root mean squared error(RMSE), normalized root mean squared error(NRMSE), coefficient of correlation(CC), Nash-Sutcliffe efficiency(NSE), and Kling-Gupta efficiency(KGE) were used to determine the best performing infiltration model and to confirm anomalies between predicted and observed values. Then we evaluated performance of five models(i.e., the Philip model, Kostiakov model, Modified Kostiakov model, Novel model, and Horton model) in simulating the infiltration process based on the adjusted performance parameters cited above. Results indicated that the Novel model had the best simulated water infiltration process in the Mitidja Plain in Algeria. However, the Philip model was the weakest to simulate the infiltration process. The conclusion of this study can be useful for estimating infiltration rate at various sites using a Novel model when measured infiltration data are not available and are useful for planning and managing water resources in the study area.展开更多
Soil infiltration properties(SIPs)of infiltration rate and saturated hydraulic conductivity significantly affect hydrological and erosion processes,thus,knowledge of SIPs under different land use/cover are vital for l...Soil infiltration properties(SIPs)of infiltration rate and saturated hydraulic conductivity significantly affect hydrological and erosion processes,thus,knowledge of SIPs under different land use/cover are vital for land use management to control soil erosion for realizing the sustainable development of the small agricultural watershed.Nevertheless,few studies have been carried out to investigate the differences in SIPs and their dominant influencing factors between different land use/cover in the black soil region of Northeast China.Therefore,eight typical land use/cover were selected to clarify the variations in SIPs between different land use/cover and further identify their dominant influencing factors.SIPs of initial infiltration rate(IIR),steady infiltration rate(SIR),and saturated hydraulic conductivity(Ks)were determined under eight typical land use/cover(forestland,shrub land,grassland,longitudinal shelterbelt,transverse shelterbelt,agricultural road,and cropland of Zea mays L.and Glycine max(Linn.)Merr)using a tension disc infiltrometer with three pressure heads of−3,−1.5,and 0 cm.The results of one-way ANOVA analysis showed that SIPs varied greatly between different land use/cover.Shelterbelt plant with Populus L.had the maximum IIR,SIR,and Ks,and then followed by shrub land,agricultural road,cropland,grassland,and forestland.Spearman correlation analysis indicated that SIPs were significantly correlated with soil and vegetation properties.Redundancy analysis revealed that differences in SIPs between different land use/cover were dominantly attributed to the differences in soil texture,field capacity,and plant root mass density,which explained 79.36%of the total variation in SIPs.Among these dominant influencing factors,the results of structural equation model indicated that the indirect effects of plant root and soil texture played the most important role in variations of SIPs via affecting soil texture and pore characteristics.These results have significant implications for the precise prediction of watershed hydrological and erosion processes,also provide a scientific basis for guiding the distribution pattern of land use in the cultivated watershed.展开更多
文摘Three types of natural soils are studied in this paper: 1) a postglacial silt, 2) a glacial till, and 3) a postglacial sand. The former two are soils from embankment dam sites in Sweden, and the latter is a soil from a natural deposit situated in the Swedish east coastal region. In situ Double-ring infiltrometer (DRI) tests are compared with laboratory constant-head permeability determinations. This study shows that the DRI tests conducted on sandy-silty soils are within sufficient range to the laboratory results, to suggest that in situ near-saturated infiltration capacity may be used as a field estimate of hydraulic conductivity (permeability) for this range of soils. In situ infiltrometer testing may be the better alternative when there is difficulty in achieving representative field conditions in a laboratory setting, e.g., for widely graded soils such as glacial tills.
基金the National Natural Science Foundation of China(grant nos.51239009,41371239)Science and Technology Planning Project of Shaanxi Province(2013kjxx-38)Natural Science of Shaanxi Province(2015JQ5161).
文摘Different land use,and associated variations in agricultural or silvicultural practices,can cause substantial variations in soils’hydraulic properties.Thus,the optimal method for measuring these properties may vary,even among neighboring sites.In this study these variations were examined by comparing measurements of hydraulic properties of soil in fields used for poplar,alfalfa and wheat cultivation obtained with two steady flow methods(the White and Sully,and single disc with multiple tension methods)and two transient flow methods(the single disc with single tension,and multiple tensions with multiple disc radius methods).The fields were all located in Changwu municipality,a major grain-producing area in Shaanxi Province,China.Disc tension infiltrometers were used to measure unconfined,unsaturated infiltration over a range of supply pressure heads(h=−9 cm,−6 cm,−3 cm and 0)at the soil surface.Intact soil cores were sampled near the surface to determine bulk density and soil water retention curves at potentials ranging from−0.15 kPa to−100 kPa.Unsaturated hydraulic conductivity values over the range of supply pressure heads were estimated using Wooding’s equation for steady-state flow from a disc source.The van Genuchten water retention model was fitted to experimental data to estimate the parameter values.The results indicated that land use affects soils’saturated and unsaturated hydraulic conductivity.Further,steady state flow methods are most appropriate for measuring hydraulic properties of soils under poplar and wheat,due to their high organic contents and saturated hydraulic conductivity.However,for soils supporting alfalfa(which are more homogeneous),instant methods provide better results,in addition to substantial time and labor savings.
基金Project supported by the Hundred Talents Program of the Chinese Academy of Sciences, the National Basic Research Program of China (No. 2005CB121103) and the National Natural Science Foundation of China (Nos. 40371057 and 50479065).
文摘A simple method was developed to relate soil sorptivity to hydraulic diffusivity and water absorption experiments were conducted utilizing one-dimensional horizontal soil columns to validate the relationship. In addition, an estimation method for hydraulic diffusivity with disc infiltrometer was developed. The results indicated a favorable fit of the theoretical relation to the experimental data. Also, the experiment with disc infiltrometer for estimating the diffusivity showed that the new method was feasible.
基金supported by the German Research Foundation (DFG)
文摘A high degree of uncertainty with regard to soil parameterisation limits the significance of physically-based simulation of distributed flood control measures, which affect the runoff generation process, such as land-use changes or differing soil tillage practices. In this study, the soil measurement data from the hillslope scale at the Scheyern research farm were compared to demonstrate this uncertainty. To account for the spatial variability of soils in the investigation area of Scheyern, different approaches were applied to estimate soil hydraulic properties and saturated hydraulic conductivity, and were compared to field measurements
文摘Soil formation is often a very slow process that requires thousands and even millions of years. Human influence, occasionally on a par with the function of climate or geological forces, can accelerate the process and can be viewed as a distinct soil forming factor. This paper describes a soil, Haplic Regosol, in which anthrosolization dominates the soil forming process. Man-made soils, Technosols, were stabilized with techniques of ecological engineering (crib walls). We measured the main soil properties and focused on the movement of water (the reduction of soil weight is the key factor in stabilizing these calcschists). The newly deposited debris, sheltered by anthropic interventions, after four years differentiated an A/C profile while after forty years differentiated an O/A/AB/Bw/BC/C profile. Our results indicate that colonization by plants and the consequent success of vegetation establishment is influenced mainly by control of the factor of pedogenesis 'topography' and by the ability of these Technosols to retain nutrients.
文摘An infiltration characteristic model was developed by using the modified Kostiakov method for the Agricultural Engineering demonstration field of Bangladesh Agricultural Research Institute (BARI). The constant values a, α, and b of the equation for accumulated infiltration y = atα + b were 9.12, 0.683, and 0.145, respectively. The average value of percentage of error between the actual and calculated values by the model was only 0.134 and showed very good agreement between the model and the field values of accumulated infiltration. This model will be very helpful for making a good irrigation scheduling and best water management.
文摘Infiltration is an important component of the hydrological cycle. It provides soil moisture in the vadose zone to support plant growth. This study was conducted to compare the validity of four infiltration models with measured values from the double ring infiltrometer. The parameters of the four models compared were estimated using the linear regression analysis. The C.C was used to show the performance of the predictability of the models. The RMSE, MAE and MBE were employed to check the anomalies between the predicted and the observed values. The results showed that, average values of the C.C ranged from 0.9294 - 0.9852. The average values of the RMSE were 4.0033, −17.489, 11.2400 and 49.8448;MAE were 3.1341, 15.9802, 10.6525, and 61.4736;and MBE were 0.0786, 9.5755, 0.0007 and 47.0204 for Philip, Horton, Green Ampt and Kostiakov respectively for the wetland soils. Statistical results also from the Fisher’s multiple comparison test show that the mean infiltration rate estimated from the Green Ampt’s, Philip’s and Horton’s model was not significantly different (p > 0.05) from the observed. The results indicated that the Kostiakov’s model had the highest deviations as it overestimated the measured data in all the plots. Comparison of the statistical parameters C.C, RMSE, MAE, and MBE for the four models indicates that the Philip’s model agreed well with the measured data and therefore, performed better than the Green Ampt’s, Horton’s and Kostiakov’s models respectively in that order for Besease wetland soils. Estimation of infiltration rate by the Philip’s model is important in the design of irrigation schemes and scheduling. Therefore, in the absence of measured infiltration data, the Philip’s model could be used to produce infiltration information for inland valley bottom soils that exhibit similar characteristic as Besease wetland soils.
基金the framework of the SWATCH project (Prima project) funded by the DGRSDT, Algeria
文摘Infiltration is an important part of the hydrological cycle, and it is one of the main abstractions accounted for in the rainfall-runoff modeling. The main purpose of this study is to compare the infiltration models that were used to assess the infiltration rate of the Mitidja Plain in Algeria. Field infiltration tests were conducted at 40 different sites using a double ring infiltrometer. Five statistical comparison criteria including root mean squared error(RMSE), normalized root mean squared error(NRMSE), coefficient of correlation(CC), Nash-Sutcliffe efficiency(NSE), and Kling-Gupta efficiency(KGE) were used to determine the best performing infiltration model and to confirm anomalies between predicted and observed values. Then we evaluated performance of five models(i.e., the Philip model, Kostiakov model, Modified Kostiakov model, Novel model, and Horton model) in simulating the infiltration process based on the adjusted performance parameters cited above. Results indicated that the Novel model had the best simulated water infiltration process in the Mitidja Plain in Algeria. However, the Philip model was the weakest to simulate the infiltration process. The conclusion of this study can be useful for estimating infiltration rate at various sites using a Novel model when measured infiltration data are not available and are useful for planning and managing water resources in the study area.
基金provided by the National Key Research and Development Program of China(2021YFD1500803).
文摘Soil infiltration properties(SIPs)of infiltration rate and saturated hydraulic conductivity significantly affect hydrological and erosion processes,thus,knowledge of SIPs under different land use/cover are vital for land use management to control soil erosion for realizing the sustainable development of the small agricultural watershed.Nevertheless,few studies have been carried out to investigate the differences in SIPs and their dominant influencing factors between different land use/cover in the black soil region of Northeast China.Therefore,eight typical land use/cover were selected to clarify the variations in SIPs between different land use/cover and further identify their dominant influencing factors.SIPs of initial infiltration rate(IIR),steady infiltration rate(SIR),and saturated hydraulic conductivity(Ks)were determined under eight typical land use/cover(forestland,shrub land,grassland,longitudinal shelterbelt,transverse shelterbelt,agricultural road,and cropland of Zea mays L.and Glycine max(Linn.)Merr)using a tension disc infiltrometer with three pressure heads of−3,−1.5,and 0 cm.The results of one-way ANOVA analysis showed that SIPs varied greatly between different land use/cover.Shelterbelt plant with Populus L.had the maximum IIR,SIR,and Ks,and then followed by shrub land,agricultural road,cropland,grassland,and forestland.Spearman correlation analysis indicated that SIPs were significantly correlated with soil and vegetation properties.Redundancy analysis revealed that differences in SIPs between different land use/cover were dominantly attributed to the differences in soil texture,field capacity,and plant root mass density,which explained 79.36%of the total variation in SIPs.Among these dominant influencing factors,the results of structural equation model indicated that the indirect effects of plant root and soil texture played the most important role in variations of SIPs via affecting soil texture and pore characteristics.These results have significant implications for the precise prediction of watershed hydrological and erosion processes,also provide a scientific basis for guiding the distribution pattern of land use in the cultivated watershed.
