1) meadow alkali soil
草甸碱土
1.
The effect of the soil conditioner MDM on ameliorating the meadow alkali soil was investigated by pot culture and field experiment.
通过盆栽及田间小区试验,研究了改良剂MDM对松嫩平原草甸碱土的改良效果。
2.
The improvement effect of desulfurized gypsum on meadow alkali soil was analyzed through field experiment, the results showed that: desulfurized gypsum could effectively decrease the pH value of meadow alkali soil and the content of exchangeable base ions which improved the conditions of soil to some degree.
通过田间试验,对脱硫石膏改良草甸碱土的效果进行了分析。
2) alkali meadow soil
碱化草甸土
1.
The effects of the alkali meadow soil treated with seedling-stimulating agentⅠand Ⅱ on the biochemical characteristics of rice seedling were studied.
研究了在碱化草甸土上施用Ⅰ型和Ⅱ型调制剂对水稻秧苗某些生化特性的影响。
3) kaline meadow soi
碱性草甸土
4) soda meadow-alkaline soil
苏打草甸碱土
1.
Soil characteristics such as soil temperature, soil moisture, soil salinity, soil pH, urease activity, hydrogeperoxidase activity were measured to evaluate the improving effects on soda meadow-alkaline soil.
本试验在黑龙江省肇州县羊泰屯进行,以畜禽粪便(鸡粪、牛粪)、鲜草为改良材料,选取pH值10以上的苏打草甸碱土为改良对象。
5) alkalized meadow
碱化草甸
1.
Dynamics of soil seed banks of two alkalized meadow communities in Songnen Plain of China;
松嫩平原碱化草甸两个群落土壤种子库动态
2.
sinensis in alkalized meadow in the Songnen Plain of china wereanalysed in this paper.
采用随机取样方法调查与测定,分析了松嫩平原碱化草甸星星草、朝鲜碱茅、獐毛3种耐盐碱禾草单优群落的生产特征。
6) meadow soil
草甸土
1.
Effect of long-term K application on potassium forms in meadow soil;
长期施用钾肥对草甸土钾素形态的影响
2.
Effect of organic manure application on the fixation of potassium in brown soil & meadow soil;
施用有机肥对棕壤和草甸土固钾作用的影响研究
3.
The meadow soil in the Zoigê Plateau could consume atmospheric CH4 at a rate of-0.
若尔盖高原草甸土氧化大气CH4的速率为-0。
补充资料:碱土
碱土 solonetz 土壤胶体中含交换性钠较多(碱化度达15%或20%)的土壤。其主要特征是:呈强碱性反应(pH8.5~11);胶体高度分散,干时收缩坚硬板结,湿时膨胀泥泞;结构性差 ,通透性不良;含盐量不高。主要分布于世界各大洲的内陆干旱、半干旱地区,常与盐土相伴存在。中国的东北、华北和西北地区多以斑块状零星分布于盐土中间。碱土因土壤胶体在吸附土壤溶液中钠离子的同时不断交换出钙、镁离子,从而使胶体中交换性钠的百分率增大。中国境内的碱土分3个亚类:①草甸碱土。多见于松辽平原和黄淮海平原,地下水较浅,土壤有轻微的季节性积盐。②草原碱土。主要在大兴安岭以西的高原草原地区,已脱离地下水影响,有明显的柱状、棱柱状碱化层。③龟裂碱土。不受地下水影响,地表因干旱呈龟裂状,几乎不能生长植物,主要在新疆、甘肃、宁夏等地的荒漠和半荒漠地带。碱土改良的中心任务是降低交换性钠的含量。施用石膏、磷石膏和氯化钙等物质,以其中的钙离子交换出碱土中的钠离子,使之随雨水和灌溉水排出土壤;施用硫磺、硫酸亚铁等酸性物质,中和土壤酸度,活化土壤中的钙,降低土壤中碳酸钠盐类浓度,提高某些矿质营养元素对植物的有效性。化学措施须与水利、农业措施相配合。
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