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The results show that not only the growth of C. wenyujin in lime soil is possible, but also the biomass, yield of medicinal part, the content of oil from the tuber and its medicinal components are higher than those from red soil. The C. wenyujin from lime soil quickly assumes etiolation during initial growth period. Surprisingly, the lusty leafs of C. wenyujin planted in red soil turn to pale and brown flecks occur in the leafs with the fertilization of N, P, K. It is concluded that C. wenyujin can be planted in lime soil; C.

结果表明:温郁金不但可以在石灰土上生长,而且其药用部位的产量、莪术油的含量及莪术油中主要药用组分β-榄香稀等的含量都较大;石灰土上生长的温郁金在生长前期较快地表现出老叶明显发黄的缺肥症状,而红壤植株在追加N、P、K 3种大量元素后功能叶子呈现黄白色,且夹带有褐色斑点的缺肥症状;石灰土中Fe元素有效态含量比红壤低一个数量级,但在石灰土上种植的温郁金植株其Fe元素含量并不比红壤上的低。

The result also showed that return treatment is better than taken treatment within different treatments. 4. According to the experiment when the plant was harvested(In March 25th,2009), it was found that the rape with NPK treatment,especially with NPK-T treatment in Quaternary red soil and in granitization red soil, grew abnormality or dead in the centre of district(80%),which yield was extremely low,but had some to the remaining(20%) close to the cement ridge.Among the three types of parent material,eighteen districts,Dischaemum Schreb of gramineae plants could only grow in granitization red soil with NPK treatment,and the other sixteen districts were little or even not.The rape planted in Quaternary red soil with NPK treatment got disease especially in the centre of the district.

其次是M处理,CK最低。3、三种母质种植油菜均表现为:归还处理好于带走处理;4、据试验收产时(2009年3月25日)发现:四纪红土和花岗岩二种母质的NPK处理的油菜除靠近水泥梗边行长有部分油菜外(占小区面积20%),小区中间(占小区面积80%)的油菜生长不正常或死亡,产量极低;三种母质共18个小区,只有花岗岩母质的NPK处理长有禾本科植物马唐草,其余16个小区很少或没有;四纪红土NPK处理油菜病害严重。

Results showed that high quality black tea was mainly produced in red soil, red yellow soil and intermountain alluvial terraces formed by fluvial outwash, with loose soil texture and high soil organic matter content.

分析表明,优质红茶产地主要是红壤、红黄壤和河流冲积形成的山间冲积台地,土壤质地疏松,有机质含量较高。

Compared carbon pools and turnovertime under different soil types, the result shows: soil total organic carbon is grey cinnamonforest soil>dark-brown soil>meadow soil>brown coniferous forest soil>red soil>yellowsoil>yellow brown soil>paddy soil>red soil>flubo-aquic soil>fengsha soil,temperate forest soil>subtropical forest soil>subtropical cropland soil>temperate dry soil.Active carbon is temperate forest soil>subtropical soil.

对不同土壤类型的碳库及其驻留时间进行比较,得出:有机碳含量呈现:灰褐土>暗棕壤>草甸土>棕色针叶林土>红壤>黄壤>黄棕壤>水稻土>农田红壤>潮土>风沙土,温带森林土壤>亚热带森林土壤>亚热带农田土壤>温带干旱土壤;活性碳含量是温带森林土壤>亚热带的土壤。

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。

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 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。

The maximum rate of decomposition of soil organic carbon insubtropical wetness area is red soil under coniferous and broad-leaved mixed forest>yellowsoil under grass>yellow soil under shrub>yellow soil under broad-leaved forest>red soilunder camellia oleifera; decomposition rate of yellow soil is faster than red soil. Themaximum rate of decomposition of soil organic carbon in subtropical wetness zone isyellow-brown soil under mixed forest in Nanjing>red soil under adult fir in Yujiang>redsoil under broad-leaved forest in Yujiang.

湿润亚热带地区森林土壤有机碳分解速率最大值出现在培养初期的一周内,其顺序:针阔混交林红壤>茅草黄壤>灌木林黄壤>常绿阔叶林黄壤>油茶红壤,同一植被下黄壤有机碳分解速率大于红壤,南京混交林黄棕壤>余江杉木(32年)红壤>余江常绿阔叶林红壤。

The results are:(1) The higher of altitude,the less of soil acidity in soil C horizon at Dinghushan;(2) There are more NH4-N,total K,available K, exchangeable K,exchangeable Na,exchangeable Mg and the content of exchangeable cations in lateritic red soil at low altitude than those in yellow soil at high altitude;(3) With increasing altitude,the contents of sio2 and Mn decrease,and the concentrations of this two minerals in lateritic red soil are higher than those in yellow soil.

结果为:(1)鼎湖山土壤剖面C层随着海拔梯度的上升,土壤酸度降低。(2)鼎湖山位于海拔低的赤红壤的NH4-N,全钾,速效钾,交换性Na,交换性钾,交换性Mg和阳离子含量比位于海拔高的黄壤的对应养分含量要高。

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What would he tell Judith and the children?

他将怎样告诉朱迪丝和孩子们呢?

I this is at that time, the opinion with peacockish true girl is full of in a heart.

这就是当时的我,一个心中布满虚荣的女孩子真实的想法。

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