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Planted vegetation, especially more than 20 years old planted trees and planted grasses consumed much more soil water than vegetation in natural restoration, and the soil water content in 200-500cm soil layers was almost near to wilting point.

相比之下,人工植被消耗大量的深层土壤水分,特别是20年龄以上的人工林地及人工草地,其200~500cm土层的土壤含水量几乎接近凋萎湿度。

Delineation result based on the improved ant clustering indicated that the study area could be partitioned into two irrigation management zones. Soil field capacity, saturation moisture content and permanent wilting point in Zone I were greater than those in Zone II, which indicated that soil in Zone I had stronger drought resistance than that in Zone II under the same climate conditions. Delineation of irrigation management zones could provide references and data support for site-specified irrigation management.

改进的蚁群聚类分区结果表明,研究区可划分成2个灌溉管理分区,I区土壤的田间持水率、饱和含水率和凋萎含水率均较II区大,表明在相同的气候条件下,I区的土壤耐旱能力较II区强,分区结果可以为精准灌溉的分区管理提供参考依据和数据支持。

The soil moisture characteristics, dynamic variation and spatial variation in the fields for 4 soils in the loess area of Gansu province, maximum hygroscopicity, wilting point moisture and water holding capacity were studied. The dynamic variation of soil moisture shows "two peaks -two valleys" type.

对甘肃黄土地区4个土类的土壤水分特征、动态及空间变异规律,以及最大吸湿水、凋萎湿度和持水性能的研究表明,土壤水分动态变异规律呈&双峰-双谷&型,据此在时序上可划分为5个明显的时期:(1)春季增失墒交替期;(2)春夏严重失墒期;(3)夏秋墒情恢复期;(4)秋冬缓慢失墒期;(5)冬季墒情稳定期。

By field and indoor test, the paper measures soil physical property, soilmoisture constant and soil water movement parameter, provides the soil specificgravity , the soil apparent density, the soil fraction, the soil field moisturecapacity, the soil saturated moisture capacity, the soil percent moisture content ofcom germination and seedlings emergence, the corn wilting point, and alsoestablishes the equation of soil water retention curves, the equation of soil waterdispersion coefficient and the relationship between pressure and soil apparentdensity, and so those provides the parameter for numerical simulation.

通过田间和室内试验,测定了供试土壤的物理性质、土壤水分常数和土壤水分运动参数,得到了该土样的比重、容重、机械组成、田间持水率、饱和含水率、玉米种子发芽出苗土壤含水率、玉米凋萎系数,给出了土壤水分特征曲线方程、土壤水分扩散系数方程及土壤容重与土壤压紧力的关系,提供了数值模拟过程中所需的参数。

The time from saturated soil moisture content to wilting percentage of Aeolian sandy soil, Loessial soil and Lou soil was extended by 244.72%,251.11% and 36.31% respectively when Sodium Polyacrylate was applied at the suggested dosage.

风砂土、黄绵土与塿土的蒸发强度随着高分子化合物聚丙烯酸钠用量增加而降低,聚丙烯酸钠用量为0.5%时,砂土、黄绵土与塿土10天累积蒸发量分别较对照降低了59.89%、48.92%与55.81%;综合考虑对土壤蓄水与蒸发能力的影响,聚丙烯酸钠用量为风砂土、黄绵土应控制在0.08%~0.2%,塿土中用量必须严格控制在0.2%左右;在上述用量条件下,风砂土、黄绵土、塿土从饱和含水量蒸发失水至凋萎含水量的时间分别被延长了244.72%、251.11%与36.31%左右。

The main results are as follows:(1) In unsteady phase, ground fissures caused by collapsing facilitate the loss of soil water. The soil water content of fissure district is about 50% less than that of non-fissure district of subsidence area, which close to or below wilting coefficient. This will be a great threat for the survival and growth of vegetation.

取得的主要进展和认识如下:(1)塌陷非稳定阶段,塌陷裂隙对土壤水分散失具有重要影响,与塌陷区非裂缝带土壤水相比,塌陷裂缝部位土壤水分损失几乎达50%,接近或低于凋萎系数,对植被生存、生长构成威胁。

Though the wilting coefficient of soil tend to increase as water-retaining agents increased,the amplitude was low, so the soil available water capacity augmented obviously.

施用保水剂后,土壤可在较长时间内保持较高的水分含量;且随保水剂用量增加,土壤容重下降,总孔隙度和毛管孔隙度则呈上升趋势;土壤凋萎系数虽有增大趋势,但增幅很小,土壤有效水容量明显增大。

The results showed that tillage had stronger compaction effect on Red soil. By analyzing retention properties, water content was higher in the same suction for Red soil. Field capacity and wilting coefficient were higher for Red soil than those for Lou soil, but effective moisture and saturated hydraulic conductivity were lower for Red soil. For Red soil, Lateral infiltration ability was stronger, infiltration rate was greater than one number degree for Lou soil and preferential flow occurred easily.

结果表明:耕作片红壤有较强的压实作用;从持水特征分析,同一吸力下红壤的含水量较高,田间持水量和凋萎系数也高于塿土,而有效水含量略低于塿土,饱和导水率却低于塿土1个数量级;从入渗特征分析,红壤的侧渗能力很强,入渗率比塿土高1个数量级,容易发生大孔隙流。

1The soil water c haracteristic curves of four soil layers in this soil were consistent. The satur ated water content, field capacity, wilting coefficient and available water capa city decreased from top soil to bottom in soil profile.(2)The unsaturated hydra ulic conductivity was significant relation with the negative pressure head in ex ponential function and tended to stable when the negative...

土壤的饱和含水量、田间持水量、凋萎系数和土壤有效水的含量均从土壤上层到下层呈降低的趋势;土壤的非饱和导水率与负压水头之间呈负相关的指数曲线变化,当负压水头达到 10 k Pa时,非饱和导水率降低到最小值,且基本趋于稳定;非饱和土壤水扩散率变化于 1.1× 10 - 3~ 1.886× 10 - 3cm2 / min之间,非饱和土壤水扩散率随含水量也呈指数曲线变化。

The saturated water content, field moisture capacity, wilting coefficient, available water, readily available water, slowly available water of experimented soils respectively has negative power, logarithmic, exponential, exponential, exponential, power, logarithmic relationship with soil bulk density.

土壤容重对土壤水分蓄持能力有较大影响,土壤蓄水能力随容重增大递减,比水容量也随容重增大递减,土壤饱和含水量、毛管断裂含水量、田间持水量、凋萎系数、有效水含量、易效水含量、迟效水含量与容重分别呈幂函数、对数、指数、指数、指数、幂函数、对数关系。

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