西安理工大学水资源研究所,西安,710048
纸质出版:2018
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曾 健, 费良军, 陈 琳, 等. 添加γ-聚谷氨酸对土壤结构及持水特性的影响[J]. 水土保持学报, 2018,32(1):217-224.
ZENG Jian, FEI Liangjun, CHEN Lin, et al. Effects of γ-PGA on Soil Structure and Water-holding Characteristics[J]. 2018, 32(1): 217-224.
曾 健, 费良军, 陈 琳, 等. 添加γ-聚谷氨酸对土壤结构及持水特性的影响[J]. 水土保持学报, 2018,32(1):217-224. DOI: 10.13870/j.cnki.stbcxb.2018.01.034.
ZENG Jian, FEI Liangjun, CHEN Lin, et al. Effects of γ-PGA on Soil Structure and Water-holding Characteristics[J]. 2018, 32(1): 217-224. DOI: 10.13870/j.cnki.stbcxb.2018.01.034.
为进一步探究γ-聚谷氨酸在农业方面应用,将不同γ-PGA含量(0,0.1%,0.2%,0.5%,1%)施入无团粒结构的砂壤土与粉壤土中,研究了γ-PGA在土壤物理结构及持水特征方面的作用。结果表明:随γ-PGA含量的增加,同一吸力下土壤持水量增加,VG模型中参数α值均大于对照组,n值递减。γ-PGA添加至1%时,砂壤土中容重降低0.087 g/cm3,孔隙度增加3.28%,粉壤土中容重降低0.108 g/cm3,孔隙度增加4.08%,添加γ-PGA降低了毛管孔隙比例,提高无效孔隙比例,表明γ-PGA对粉壤土物理特性影响大于砂壤土。饱和含水量与γ-PGA含量呈幂函数正相关,饱和扩散率则呈负相关关系,粉壤土中VG模型参数所计算饱和扩散率与水平入渗法计算值间相对误差值小于10%。除凋萎系数外,γ-PGA对其余土壤水分常数影响显著,均随γ-PGA含量增加而增大。土壤中薄膜水、毛管水比例提高,重力水比例显著下降。γ-PGA含量为1%时,粉壤土中有效水比例为64.83%,砂壤土中仅为56.14%。添加γ-PGA有利于改良土壤内孔隙分布,提高持水能力,防止土壤水分的深层渗漏。
In order to further research the application of γ-PGA in agriculture
different contents of γ-PGA (0
0.1%
0.2%
0.5% and 1%) were applied in sandy loam and silty loam without granular structure to study the effects of γ-PGA on soil physical structure and water retention characteristics. Results showed that: with the increasing of γ-PGA content
water retention capacity of soil increased under the same absorption force. Values of α in the VG model were all larger than those in the control group
and n value decreased progressively. When the content of γ-PGA increased to 1%
the bulk density of sandy loam decreased by 0.087 g/cm3
and the porosity increased by 3.28%; corresponding parameters of silty loam were 0.108 g/cm3 and 4.08%
respectively. The addition of γ-PGA reduced the proportion of capillary pore
and increased the proportion of invalid pore
indicating that effect of γ-PGA on the physical characteristic of silty loam were greater than those of sandy loam. Power function positive correlation existed between the saturation moisture content and the γ-PGA content
while negative correlation existed between the saturation diffusion rate and the γ-PGA content. The relative error between the saturation diffusion rates calculated by parameters of VG model and horizontal infiltration method was smaller than 10% in silty loam. Except for the wilting coefficient
γ-PGA had significant effects on other soil water constants
wherein the constants increased with the increasing of γ-PGA content. In the soil
proportions of film water and capillary water increased
whereas the proportion of gravitational water decreased significantly. When the γ-PGA content was 1%
the proportion of available water was 64.83% in silty loam
whereas the value was only 56.14% in sandy loam. Adding γ-PGA was beneficial to improve pore distribution in soil and water retention capacity
and prevent deep seepage of soil moisture.
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