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枯草芽孢杆菌改良盐碱土过程中水盐运移特征
引用本文:周蓓蓓,侯亚玲,王全九.枯草芽孢杆菌改良盐碱土过程中水盐运移特征[J].农业工程学报,2018,34(6):104-110.
作者姓名:周蓓蓓  侯亚玲  王全九
作者单位:1. 西安理工大学 西北旱区生态水利工程国家重点实验室培育基地,西安 710048;,1. 西安理工大学 西北旱区生态水利工程国家重点实验室培育基地,西安 710048;,1. 西安理工大学 西北旱区生态水利工程国家重点实验室培育基地,西安 710048;2. 中国科学院水利部水土保持研究所 黄土高原土壤侵蚀与旱地农业国家重点实验室,杨陵 712100
基金项目:国家自然科学基金重点项目(51239009,41371239);陕西省科技支撑项目(2013KJXX-38);西安理工大学特色研究计划项目(2016TS013)
摘    要:该文通过室内一维土柱试验,设置5种不同枯草芽孢杆菌质量分数(0、1、3、5、7 g/kg)处理,研究不同含量枯草芽孢杆菌对盐碱土水盐运移的影响。结果表明:施加枯草芽孢杆菌后,土壤累积入渗量、入渗速率及湿润锋运移距离均显著降低,在入渗时间为3 600 min时,枯草芽孢杆菌质量分数为1、3、5、7 g/kg的累积入渗量相比0 g/kg分别减少了18.49%、21.85%、12.18%、3.78%;当湿润锋运移至27 cm时,枯草芽孢杆菌含量为1、3、5、7 g/kg所用时间相比0 g/kg分别增大了96.21%、108%、37.84%、16.76%,在枯草芽孢杆菌施加量为3 g/kg时,单位入渗历时内累积入渗量、入渗速率及湿润锋的运移距离最小。枯草芽孢杆菌同样影响Philip方程和Green-Ampt入渗公式参数显著,土壤水饱和导水率KS、吸渗率S、稳定入渗率A随着枯草芽孢杆菌含量的增加先减少后增大,湿润锋处的吸力hf先增大后减少,当施加量为3 g/kg时,S、KS、A均取得最小值,hf取得最大值。枯草芽孢杆菌可提高土壤的保水性能,在土层深度为27 cm处,施加量为1、3、5和7 g/kg相比0 g/kg的剖面含水量分别增加了17.65%、31.76%、11.76%、7.06%。施加枯草芽孢杆菌的土壤在入渗结束后,土壤的含盐量分别降低了22.37%、31.29%、17.78%、10.67%。施加枯草芽孢杆菌后,1、3、5、7 g/kg的水稳性团聚体含量相比0 g/kg分别增加了13.02%、17.59%、9.68%和5.24%。综上,在盐碱土中施加3 g/kg的枯草芽孢杆菌,对盐碱土壤的治理具有积极作用。

关 键 词:入渗  土壤水分  含盐量  枯草芽孢杆菌  盐碱土  团聚体
收稿时间:2017/9/21 0:00:00
修稿时间:2018/2/18 0:00:00

Characteristics of water and salt migration in process of improving saline alkali soil with bacillus subtilis
Zhou Beibei,Hou Yaling and Wang Quanjiu.Characteristics of water and salt migration in process of improving saline alkali soil with bacillus subtilis[J].Transactions of the Chinese Society of Agricultural Engineering,2018,34(6):104-110.
Authors:Zhou Beibei  Hou Yaling and Wang Quanjiu
Institution:1. State Key Laboratory Base of Eco-hydraulic Engineering in Arid Area, Xi''an University of Technology, Xi''an 710048, China;,1. State Key Laboratory Base of Eco-hydraulic Engineering in Arid Area, Xi''an University of Technology, Xi''an 710048, China; and 1. State Key Laboratory Base of Eco-hydraulic Engineering in Arid Area, Xi''an University of Technology, Xi''an 710048, China; 2. State Key Laboratory of Soil Erosion and Dryland Farming on the Loess Plateau, Institute of Soil and Water Conservation, Chinese Academy of Sciences and Ministry of Water Resources, Yangling 712100, China
Abstract:Abstract: Bacillus subtilis has great effects on soil water and salt movement. In this paper, 5 different contents of Bacillus subtilis (0, 1, 3, 5 and 7 g/kg) were set, aiming to study the soil water cumulative infiltration, infiltration rate, wetting front, soil water contents and salt contents in each profile, as well as water-stable aggregate contents. The results showed that with the applying of Bacillus subtilis, the cumulative infiltration and infiltration rate in saline-alkali soil decreased obviously, compared to that in the control of soil columns, due to the water retention properties of Bacillus subtilis, especially after the initial 300 min. Moreover, with the increase of Bacillus subtilis content, the cumulative infiltration and infiltration rate first decreased and then increased. When the Bacillus subtilis content was 3 g/kg, the cumulative infiltration and infiltration rate of soil water tended to be the smallest in a certain time, and the variations between the treatments were significant (P<0.01). At the end of the infiltration, the cumulative infiltration with the Bacillus subtilis content of 1, 3, 5 and 7 g/kg was decreased by 18.49%, 21.85%, 12.18% and 3.78% respectively compared with that without Bacillus subtilis. With the applying of Bacillus subtilis, the wetting front decreased as well. At the initial time, there were no significant differences between different treatments. With the infiltration time increasing, the effect of Bacillus subtilis on wetting front in each treatment was significant (P<0.01). The wetting front took 3 700, 7 260, 7 700, 5 100 and 4 320 min to reached the bottom of the soil column with Bacillus subtilis content of 0, 1, 3, 5 and 7 g/kg, respectively, and the migration rates were 7.84×10-3, 4.00×10-3, 3.77×10-3, 5.69×10-3, and 6.71×10-3 cm/min, accordingly. When the content was 3 g/kg, the migration rate of wetting front was the smallest. Both Philip and Green-Ampt model could fit soil infiltration process well with different Bacillus subtilis contents. For Green-Ampt infiltration model, with the increase of Bacillus subtilis contents, soil water saturated hydraulic conductivity first decreased and then increased, and the wetting front suction showed an opposite trend compared with control treatment (P<0.05). For the Philip infiltration model, with the increase of Bacillus subtilis contents, the soil sorptivity and stable infiltration rate first decreased and then increased, which were obviously less than that without Bacillus subtilis (P<0.05). When the Bacillus subtilis was 3 g/kg, the minimum values of soil sorptivity, soil water saturated hydraulic conductivity and stable infiltration rate were obtained, and the maximum value of wetting front suction was obtained, which further confirmed that Bacillus subtilis could increase soil water holding capacity. When the Bacillus subtilis contents were 1, 3, 5 and 7 g/kg, the water contents were greater than that in control. At the depth of 27 cm, the water content in the treatments with Bacillus subtilis of 1, 3, 5 and 7 g/kg increased by 17.65%, 31.76%, 11.76% and 7.06% respectively, compared with that in control. Soil salt contents were also significantly decreased with the application of Bacillus subtilis. The salt content in the treatments with Bacillus subtilis of 1, 3, 5 and 7 g/kg decreased by 22.37%, 31.29%, 17.78% and 10.67% respectively, compared to that in control. After applying Bacillus subtilis, soil water-stable aggregate also increased. In the whole soil layer, the water-stable aggregates in the treatment with Bacillus subtilis of 1, 3, 5 and 7 g/kg were greater than those in control, and increased by 13.02%, 17.59%, 9.68% and 5.24%, respectively. This study can provide a theoretical support for the microorganism application in saline-alkali soil amendment.
Keywords:infiltration  soil water  saltness  Bacillus subtilis  saline-alkali soil  aggregate
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