1) Lou soil
(土娄)土
1.
Lou soil(a well developed agricultural soil) in Loess Plateau can be sorted as a subgroup under the eum-orthic anthrosois in the Chinese Soil Taxonomy(Revised Proposal).
黄土高原(土娄)土在《中国土壤系统分类(修订方案)》中属土垫旱耕人为土类的相应亚类,其土壤水分状况是诊断表层所属人为表层类堆垫表层(覆盖层)和诊断表下层(黏化层)的重要诊断特征。
2.
Using batch experiment,the adsorption kinetics of phenol on both tillage layer(TL) and clay layer(CL) of Lou soil modified with cetyltrimethylammonium bromide(CTMAB,CB) at various ratio(100 CB and 50 CB)and cetyltrimethylammonium bromide+sodium dodecylsulphonate(CTMAB+SDS,CS) mixture were carried out, and its mechanism was discussed also.
以十六烷基三甲基溴化铵单一修饰(CB)和十六烷基三甲基溴化铵+十二烷基磺酸钠混合修饰(CS)(土娄)土耕层和黏化层土样,采用批处理法通过不同的速度参数研究了修饰土样对苯酚的吸附动力学特征,并对其机制进行了探讨。
2) old manured loessal soil
土娄土
1.
Studies on the adsorption of cetyltrimethylammouium bromide(CTMAB) in old manured loessal soil;
(土娄)土对十六烷基三甲基溴化铵的吸附研究
3) Lou soil
土娄土
1.
The results obtained in one year showed that the seasonal dynamics of soil respiration rate in Lou soil was obvious and relatively complex,and its maximum value appeared in the first ten days of July,while the lowest in winter.
结果表明,(土娄)土农田土壤的呼吸速率呈明显的季节性变化,以7月上旬最大,冬季最小;土壤温度是影响土壤呼吸速率的主要因素,二者间存在极显著的幂函数相关关系(P<0。
2.
Effects of water and temperature on the N_2O emission and the preliminary mechanism of the soil N_2O emission were studied in terms of the kinetic theory of chemical reactions in the Lou soil-a typically cultivated soil in arid and semiarid region in the Northwester of China.
本文通过室内试验研究了西北地区的典型耕种土壤(土娄)土中N2O在不同水温变化下的释放特征,借助化学反应动力学理论对其释放机理进行了初步的探讨。
4) Lou soil area
土娄土区
1.
Response of different vegetable to K fertilizer on Lou soil area;
(土娄)土区不同蔬菜对钾肥的肥效反应
5) tilled surface lou-soil
耕层土娄土
6) Earth-cumulic Orthic Anthrosols (Lou soil)
土垫旱耕人为土(土娄土)
补充资料：[3-(aminosulfonyl)-4-chloro-N-(2.3-dihydro-2-methyl-1H-indol-1-yl)benzamide]
分子式：C16H16ClN3O3S
分子量：365.5
CAS号：26807-65-8
性质：暂无
制备方法：暂无
用途：用于轻、中度原发性高血压。
分子量：365.5
CAS号：26807-65-8
性质：暂无
制备方法：暂无
用途：用于轻、中度原发性高血压。
说明：补充资料仅用于学习参考，请勿用于其它任何用途。
参考词条