兰州理工大学 能源与动力工程学院,甘肃,兰州,730050
纸质出版:2016
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赵文举, 郁文, 范严伟, 等. 滴灌条件下容重对压砂土壤水分入渗规律的影响[J]. 水土保持通报, 2016,36(1):169-173.
ZHAO Wenju, YU Wen, FAN Yanwei, et al. Influences of Soil Bulk Density on Point Source Infiltration Pattern Under Drip Irrigation Condition in Gravel-sand Mulch Soil[J]. Bulletin of Soiland Water Conservation, 2016, 36(1): 169-173.
赵文举, 郁文, 范严伟, 等. 滴灌条件下容重对压砂土壤水分入渗规律的影响[J]. 水土保持通报, 2016,36(1):169-173. DOI: 10.13961/j.cnki.stbctb.2016.01.029.
ZHAO Wenju, YU Wen, FAN Yanwei, et al. Influences of Soil Bulk Density on Point Source Infiltration Pattern Under Drip Irrigation Condition in Gravel-sand Mulch Soil[J]. Bulletin of Soiland Water Conservation, 2016, 36(1): 169-173. DOI: 10.13961/j.cnki.stbctb.2016.01.029.
[目的
]
研究土壤容重对压砂地点源入渗的影响规律
为西北旱区发展砂地滴灌技术提供实际理论依据. [方法
]
通过室内模拟土槽试验
以裸地(无植被和压砂)为对照组(CK)
研究了土壤容重(1.23
1.38
1.53 g/cm
3
)对不同种植年限压砂地(新压砂地、中压砂地、老压砂地)砂石层和土壤层两相介质点源入渗规律的影响. [结果
]
压砂土壤点源垂直累积入渗与其容重和种植年限皆呈负相关关系
压砂土壤在入渗初期
容重对其入渗深度无明显影响
当入渗到达土壤后
入渗深度明显受到容重的影响
容重越大
入渗深度越小;CK水平入渗距离随容重增加而增加
压砂土壤水平入渗随容重增加的变化无明显规律.用λ表征湿润体纵横比
CK和压砂土壤的λ总体随土壤容重增加而减小
压砂土壤容重相同时
λ随种植年限增加而减小.CK入渗前期λ随入渗时间的增加而增加
后期趋于平缓;压砂土壤λ入渗初期随时间增加显著增大
当入渗到达土壤时λ减小
中后期随入渗时间增加λ缓慢增长直至变化不明显. [结论
]
压砂对土壤水分垂直入渗有促进作用
压砂土壤点源垂直累积入渗与其容重和种植年限皆呈负相关关系.
[Objective] The influences of soil bulk density on point source infiltration in gravel-sand mulched field were studied in order to provide basis for the development of drip irrigation technique in sandy area. [Methods] Bare land(no vegetation and sand mulch) was selected as the contrast group(CK). Based on laboratory simulation experiment
this article studied the influences of different soil bulk density(1.23 g/cm3
1.38 g/cm3
1.53 g/cm3) on point source infiltration pattern in gravel-sand with different planting years(new gravel-sand mulched field
middle gravel-sand mulched field
old gravel-sand mulched field). [Results] The point source vertical cumulative infiltration showed a negative correlation with soil bulk density and planting years. Soil bulk density showed no significant effect on the infiltration depth in the initial period of infiltration. While infiltration depth were significantly influenced by the density as the infiltration reached the soil
and bulk density decreased with the increase of infiltration depths. Horizontal infiltration distance of CK increased with the increase of soil bulk density
while the change of horizon infiltration of gravel-sand mulched field was not obvious. The moist body aspect ratio was represented with λ
the λ of CK and sand mulch soil decreased with the increase of soil bulk density. When sand mulch soil bulk density was constant
λ decreased with the increase of planting years. The λ of CK increased with the increase of infiltration time in the initial days of infiltration and then became stable. The λ of sand mulch soil increased significantly with the increase of infiltration time in the initial minutes of infiltration
while it decreased when infiltration reached the soil
and the increase of λ was not obvious in the late minutes. [Conclusion] Gravel-sand mulch promote the vertical cumulative infiltration of soil moisture
and point source vertical cumulative infiltration show a negative correlation with soil bulk density and planting years.
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