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An experiment of interplan ting herbage in red soil to improve these shortcomings was carried out.

试验在红壤上种植牧草4-7年后,红壤的上述症状都得到了不同程度的改良,效果显著。

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。

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。

While it is contrary that the more contents of Fe,Ca and P are in yellow soil at higher altitude than those in lateritic red soil;(4) The pine forest has the highest content of Pb,and the Pb content is higher in soil at low altitude than that in high altitude.

鼎湖山土壤二氧化硅,锰含量随着海拔梯度的上升而下降,赤红壤含量高于黄壤;然而铁含量则随着海拔梯度的上升呈上升趋势,赤红壤含量低于黄壤,钙全量含量和磷含量也是赤红壤低于黄壤。(4)土壤Pb马尾松林含量最高,随着海拔梯度上升含量有下降趋势。

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

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。

The study on the inherent relations of microbial biomass in red soil with soil nutrient cycling and ryegrass growth shows that the microbial biomass was not only significantly correlated with soil organic C, total N and available N, but also highly correlated with dry matter yield and N uptake of plants,indicating that soil microbial biomass could be used as an important indicator for soil fertility and plant production.

研究了红壤微生物量与土壤养分循环及植物生长的内在联系。结果表明,红壤微生物量不仅与土壤有机碳、全氮、有效氮等显著相关,而且与植物干物质产量及吸N 量也存在着良好的相关性,可作为指示红壤肥力水平和作物产量的重要指标。

Ammonia volatilization in relation to N application rate and climate factors was studies through field experiment in red soil under the crop rotation of Smooth Crabgrass in spring and Winter Radish in autumn Results indicate that ammonia volatilization in Treatments N90, N160 and N230 in spring dragged on for 10~17 days, and peaked at the 6th~8th day after urea application, reaching N0.11, 0.57 and 1.84kg hm^(-2)d^(-1), respectively, and the total amount of N loss through ammonia volatilization was N0.67~5.16kg hm^(-2) accounting for 0.74%~2.24% of the total N applied.

通过红壤旱地种植牧草马唐和蔬菜冬萝卜轮作试验,研究了在春秋二季红壤旱地氨挥发对不同施氮量和气象因子的响应。结果表明,红壤旱地春季牧草实验,氮肥处理N90、M60和N230,氨挥发持续10~17d,在施肥后6~8d达到峰值,峰值分别为N0.11、0.57和l.84kg hm^(-2)d^(-1)。

The results showed that tillage had stronger compaction effect on Red soil. By analyzing retention properties, water content was higher in the same suction for Red soil. Field capacity and wilting coefficient were higher for Red soil than those for Lou soil, but effective moisture and saturated hydraulic conductivity were lower for Red soil. For Red soil, Lateral infiltration ability was stronger, infiltration rate was greater than one number degree for Lou soil and preferential flow occurred easily.

结果表明:耕作片红壤有较强的压实作用;从持水特征分析,同一吸力下红壤的含水量较高,田间持水量和凋萎系数也高于塿土,而有效水含量略低于塿土,饱和导水率却低于塿土1个数量级;从入渗特征分析,红壤的侧渗能力很强,入渗率比塿土高1个数量级,容易发生大孔隙流。

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