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281.
以盐碱土和盆栽野生大豆为研究对象,测定土壤中N、Na+、K+、Ca2+、Mg2+、Cl-、HCO3-、SO42-、CO32-和野生大豆根、茎叶、种子的氮含量,研究野生大豆对盐碱土的影响。结果表明:野生大豆能够提高盐碱土的氮含量。在花期和收获期土壤氮含量比原盐碱土分别提高了98和113%。野生大豆能够有效降低盐碱土的各种水溶性盐离子的含量和总量。在收获期土壤Na+、Cl-、HCO3-和SO42-含量比原盐碱土分别降低了94.9、85.3、47.6和95.5%;土壤可溶性盐离子总量比原盐碱土降低了90.5%。野生大豆对于盆栽盐碱土有改良作用。在收获期,野生大豆地上部分生物量很大,且在各个生长期的盐度下都能很好生长,具有绿化盐碱地的作用。 相似文献
282.
283.
Soil aggregate (SA) can be formed and stabilized when soil organic matter (SOM) is decomposed in the soil. However, the relationships between the SA dynamics and SOM with different decomposition rates have not been clarified. Therefore, this study examined the effects of the addition of polysaccharides to soil on SA formation and stability. A Japanese tropical soil was incubated for 99 d at 30 °C in a dark environment following the addition of 0.5% (w/w) starch or cellulose. The decomposition rates of the amendments, and SA formation and stability were evaluated by measuring soil respiration rates, and distribution fractions of soil aggregate sizes and mean weight diameter (MWD) of SA, respectively. The cumulative soil respirations with all treatments rapidly increased until Day 12 of the incubation. The initial slope of the cumulative soil respiration in the soil with starch was significantly higher than that in the soil with cellulose. In either soil with starch or cellulose, the fractions of macro-aggregates (>1000 μm in diameter) significantly increased, respectively, compared with control soil. However, the fractions of meso-aggregates (250–1000 μm) and nano-aggregate (<20 μm) in the soil with starch significantly decreased, while those fractions in the soil with cellulose fluctuated until Day 6. The MWDs reached the maximum on Day 6, indicating the SA formation in the soils with starch or cellulose. The increasing rate of the SA formation in the starch-amended soil was greatly higher than that in the cellulose-amended soil. After Day 6, the MWDs in the soils with either polysaccharide decreased with similar trends with no significant differences between treatments, indicating similar stability of the SA in both treatments. This study showed that the different decomposability of the organic amendments might influence the SA formation differently, but not the SA stability. 相似文献
284.
风沙土水分入渗与再分布过程中湿润锋运移试验研究 总被引:2,自引:0,他引:2
利用室内模拟试验系统,对塔克拉玛干沙漠腹地风沙土在滴灌条件下的水分入渗与水分再分布过程中湿润锋的运动规律进行了模拟试验研究。根据模拟试验描述了风沙土在滴灌条件下水分入渗与再分布情况下湿润体的形状变化,研究了在水平方向上与垂直方向上风沙土的湿润锋推进规律及运动特征,揭示了随着累计入渗量的增加,湿润锋推进过程在入渗初期速率较大,逐渐成减小趋势,并最终达到稳定入渗状态;在土壤水分再分布过程中土壤湿润锋面不断向外部推移,最后达到相对稳定;对风沙土水分入渗及再分布过程中其湿润锋的推进距离与时间做了函数关系拟合,其中乘幂函数关系式拟合最好。 相似文献
285.
The phosphate in the soil-root interface zone under various soil water contents and application rates of phosphate was still of depletion distribution which could be described by a power function in the form of C/Co= axb(C/Co is the relative content of fertilized phosphate in a distance from the root surface x, a and b are the regression constants). The depletion rate of phosphate in soil near the root surface was higher and the depletion range was narrower under lower soil moisture. On the contrary, at higher soil water content the depletion range was wider, generally. The application rate of phosphate led to the greater depletion intensity of phosphorus was higher in the heavier texture soils. In general, the depletion intensity in the soils, which decreased with increasing clay content or increasing buffering power of soil, decreased in the order as loessal soil and black lou soil > lou soil > yellow cinnamon soil when 50 or 100 mg of phosphorus were applied in the form of KH2PO4. This result indicated that the phosphate distribution and its movement in the soil-root interface zone closely related with the buffering capacity of soil. 相似文献
286.
We up-scaled the APSIM simulation model of crop growth, water and nitrogen dynamics to interpret and respond to spatial and temporal variations in soil, season and crop performance and improve yield and decrease nitrate leaching. Grain yields, drainage below the maximum root depth and nitrate leaching are strongly governed by interaction of plant available soil water storage capacity (PAWC), seasonal rainfall and nitrogen supply in the water-limited Mediterranean-type environment of Western Australia (WA). APSIM simulates the interaction of these key system parameters and the robustness of its simulations has been rigorously tested with the results of several field experiments covering a range of soil types and seasonal conditions in WA. We used yield maps, soil and weather data for farms at two locations in WA to determine spatial and temporal patterns of grain yield, drainage below the maximum root depth and nitrate leaching under a range of weather, soil and nitrogen management scenarios. On one farm, we up-scaled APSIM simulations across the whole farm using local weather and fertiliser use data and the average PAWC values of soil type polygons. On a 70 ha field on another farm, we used a linear regression of apparent soil electrical conductivity (ECa) measured by EM38 against PAWC to transform an ECa map of the field into a high resolution (5 m grid) PAWC map. We then used regressions of simulated yields, drainage below the maximum root depth and nitrate leaching on PAWC to upscale the APSIM simulations for a range of weather and fertiliser management scenarios. This continuous mapping approach overcame the weakness of the soil polygons approach, which assumed uniformity in soil properties and processes within soil type polygons. It identified areas at greatest financial and environmental risks across the field, which required focused management and simulated their response to management interventions. Splitting nitrogen applications increased simulated wheat yields at all sites across the field and decreased nitrate leaching particularly where the water storage capacity of the soil was small. Low water storage capacity resulted in both low wheat yields and large leaching loss. Another management option to decrease leaching may be to grow perennial vegetation that uses more water and loses less by drainage.Paper from the 5th European Conference on Precision Agriculture (5ECPA), Uppsala, Sweden, 2005 相似文献
287.
Chemical reactions and fate of the toxins of Bacillus thuringiensis(Bt) in the soil environment are causing increasing concerns due to the large-scale cultivation of transgenic Bt plants.In this study,the effect of ionic strength(0-1 000 mmol kg 1) adjusted by NaCl or CaCl 2 on adsorption of Bt toxin by a lateritic red soil,a paddy soil and these soils after chemical removal of organic-bound or free Fe and Al oxides,as well as by pure minerals(goethite,hematite and gibbsite) which are widespread in these soils,were studied.The results indicated that when the supporting electrolyte was NaCl,the adsorption of Bt toxin by the lateritic red soil and paddy soil increased rapidly until the ionic strength reached 250 mmol kg 1 and then gradually slowed down with the increase of ionic strength;while in case the supporting electrolyte was CaCl 2,the adsorption of Bt toxin enhanced significantly at low ionic strength(< 10 mmol kg 1) and then decreased as the ionic strength increased.The adsorption of Bt toxin by the tested minerals and soils after the removal of organic-bound or free Fe and Al oxides also increased with increasing ionic strength controlled by NaCl.Removing organic-bound Fe and Al oxides obviously increased the adsorption of Bt toxin in the tested soils.Differently,removing free Fe and Al oxides increased the Bt adsorption by the paddy soil,but decreased the adsorption by the lateritic red soil.The study indicated that the varieties of ionic strength and the presence of Fe and Al oxides affected the adsorption of Bt toxin by the soils,which would contribute to the further understanding of the fate of Bt toxin in the soil environment and provide references for the ecological risk assessment of transgenic Bt plants. 相似文献
288.
滨海地区受台风影响,降雨有其特殊性。滨海火电厂的建设,涉及山体开挖,滩涂围填,陆域海域防洪,交通运输,循环水和淡水供(排)水管(沟)布设,灰渣场、施工区、取土弃土场选址以及移民安置等诸方面问题,地形复杂,工程量大,建设期及生产运行期都极易造成严重的水土流失。以福建大唐宁德火电厂一期工程为例,分析其水土流失的特点,并提出切实可行的防治措施。 相似文献
289.
利用人工污染土壤,研究了高锰酸钾对4种不同土壤中菲和芘的氧化修复效果。结果表明,当高锰酸钾浓度为33.33mmol·L^-1时,土壤中菲和芘的氧化去除率达到最大。高锰酸钾氧化去除率不仅与高锰酸钾浓度有关,还与土壤性质和老化时间有关。土壤有机质含量的增加会降低高锰酸钾对土壤中菲和芘的氧化去除率;随着老化时间的增加,高锰酸钾的氧化去除率逐渐降低。老化40d后,4种土壤中菲和芘的氧化去除率显著降低,菲的氧化去除率在14%~67%之间,芘的氧化去除率在61%~84%之间。高锰酸钾氧化前后,4种土壤中有机质含量下降范围为0.77%~9.21%。从土壤有机质含量来看,高锰酸钾氧化修复多环芳烃污染土壤对土壤质量影响较小,具有较好的应用前景。 相似文献
290.
为了满足提高农业经济效益和生态效益的要求,研究开发了基于WebGIS的农田土壤推荐施肥信息系统.该系统将因特网和GIS技术相结合,应用于农田土壤推荐施肥服务,具有很强的数据采集、施肥信息查询、专题分析、施肥决策、后期预测等功能;人机界面十分友好,可视化程度高,操作简便;通用性好,适用于不同地区的农田土壤推荐施肥服务. 相似文献