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砖红壤

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Under the same condition,the maxi-um 〓 adsorption for goethite was 3,3.5,and 8 times as kaolinite,bayeriteand gibbsite respectively,and also the maxium 〓 adsorption of YB colloid was1.4,3,and 7 times as that of 〓 LR colloids respectively.

同样条件下针铁矿对〓的最大吸附量分别相当于高岭石、三羟铝石、三水铝石的3,3.5,8倍;黄棕壤胶体对〓的最大吸附量相当于红壤胶体〓的1.4倍,红壤胶体〓的3倍,砖红壤的7倍。

Cl - adsorption,metal cation adsorption,inducing adsorption,variable charge soil,constant charge soil.

本文主要研究在可变电荷土壤和恒电荷土壤中,金属阳离子对Cl-离子吸附的诱导效应。1 实验部分1 1 土壤样本土壤样本为广东省的砖红壤和赤红壤,江西省的红壤以及江苏省的黄棕壤,均为底土。

This research studies the effects of mineral oil of Lateritic Red Earth and Laterite on the paddy's and peanut's physico-ecologies and the reduction of mineral oil in these soils by the pot-planting simulation test.

本研究采用盆栽试验法,研究了赤红壤、砖红壤中矿物油对水稻、花生的生理生态影响和矿物油在土壤中的净化。

The major results of the work are summarized as follows: In the tested pH values, the ratios of positive charge densities to the negative charge densities of latosol particles were in the range of 0.4 to 0.8, the Po./Ne. of lateritic red soil particles were in the range of 0.08 to 0.22, whereas the Po.

主要研究结果如下:在测试pH条件下,砖红壤悬液中正电荷密度占到负电荷密度的40 -80 %,赤红壤悬液中为8.4 - 22 %,红壤悬液为1.6 - 6.4 %;在红壤悬液中可以忽略正电荷的影响。

The Wien effects of three variable charge soils (red soil, lateritic red soil and latosol) saturated with various chlorides in electric field were different. The relative electrical conductivities of red soil saturated with various chlorides increased apparently with the increase in field strength, whereas that of latosol were almost equal to 1 in the test field strength (15 kV cm-1 to 250 kV cm-1), the increase of △EC in lateritic red soil were between that of red soil and latosol.

各氯化物饱和红壤悬液的相对电导率随着场强的增加而明显增大,且不同的氯化物饱和悬液的△EC之间差异明显;砖红壤悬液的△EC随着场强的增加没有出现变化,在所测场强下(15 kV cm -1到250 kV cm -1)各悬液的△EC都几乎为1;而赤红壤悬液中的现象处于前两者之间。

The Wien effects of three variable charge soils (red soil, lateritic red soil and latosol) saturated with various chlorides in electric field were different. The relative electrical conductivities of red soil saturated with various chlorides increased apparently with the increase in field strength, whereas that of latosol were almost equal to 1 in the test field strength (15 kV cm-1 to 250 kV cm-1), the increase of △EC in lateritic red soil were between that of red soil and latosol.

各氯化物饱和红壤悬液的相对电导率随著场强的增加而明显增大,且不同的氯化物饱和悬液的△EC之间差异明显;砖红壤悬液的△EC随著场强的增加没有出现变化,在所测场强下(15 kV cm -1到250 kV cm -1)各悬液的△EC都几乎为1;而赤红壤悬液中的现象处于前两者之间。

Mineral Oil Lateritic Red Earth Laterite Residue Critical Content and Reduction

矿物油;赤红壤;砖红壤;残留;临界含量;净化

So the higher temˉ perature resistance for the three soil types was in the sequence o f dry red soil, lateritic red soil and lateritic soil.

综合3种配方在高温期间的生理指标变化情况,其耐高温能力由强到弱依次为:燥红壤、赤红壤、砖红壤

The infrared spectra of latosol and red soil fall into the kaolinite spectrum. On the other hand, the infrared spectra of yellow brown soil, lou soil, heilu soil, loessal soil fall into the montmorillonite spectrum.

结果表明,砖红壤、红壤红外光谱属于高岭石型图谱,显著的3695,3620,1035cm^(-1)峰以及3527cm^(-1)峰可作为用红外光谱判断热带、南亚热带地带性土壤的特征峰。

Result shows that the weathering rates were very low (usually lower than 1.0 keq × ha-1× a-1) for allite (including red earth, lateritic red earth, red earth, yellow earth, and yellow-brown earth) in south China and silalsol (consisting of dark brown forest soil, black soil, and podzolic soil) in northeast China, but very high for xerosol and alpine soil in northwest China.

总的说来,中国南方富铝土区域(包括砖红壤带、赤红壤带、红壤黄壤带和黄棕壤带)以及东北的硅铝土区域(包括暗棕壤黑土带和漂灰土带)的土壤风化速率较低(通常低于1.0 keq × ha-1× a-1),而西北地区干旱土和高山土的风化速率则较高。

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