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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。

Secondly, I study the expermets about the heat-moisture migration, analyze moisture transfer and correlation theory of the temperature field in the frozen soil , analysis comparally the temperatue field ,the moisture field, dynamical sources , and the water transport rate and so on of the moisture and temperature transfer both in the soft rock materical and in the frozen soil, gained the consistency and the difference in the heat-moisture migration about the soft rock materical and the frozen soil under the same condtion, the heat-moisture migration of the soft rock materical is accord with the correlation theory of the capillary porous colloid's heat and mass transfer, the theory caused moisture transfer of frozen soil is applied samely in the soft rock materical.

其次,研究冻土相关的水热迁移实验,分析了冻土水分迁移及温度场相关的规律;通过与冻土水热迁移对比分析软岩类材料的水热迁移的温度场、水分场、动力源和水分迁移速度等,得出了软岩类材料与冻土在同一条件下的水热规律的一致性和差异性,软岩类材料水热迁移也符合毛细孔隙胶体介质之热-质迁移的相关理论,引起冻土水分迁移的吸附-薄膜理论依然适用软岩类材料。

In Eucalyptus forestland, soil organic carbon, total nitrogen, available potassium contents and soil PH decreased significantly; soil available phosphorus and exchangeable magnesium contents, net nitrogen mineralization rate and ammonification rate also decreased but showed no significant difference. In shrubland, soil exchangeable calcium content increased significantly, but the contents of other nutrients had no significant change.

结果表明:火烧3年后,桉林土壤有机碳、全氮、速效钾和pH含量明显降低,土壤有效磷、交换性镁、土壤净氮矿化速率和氨化速率降低,但不显著;火烧灌草坡除土壤交换性钙明显增加外,其他土壤养分均无显著变化。

Study on 6 soil enzyme activities and 7 siol fertility factors of 12 different planting modes,analyse the dates with the correlation analysis and the canonical correalation analysis,In order to reveal the relations between the soil enzyme activities and soil fertilities in the low hill lands along Yantze River , The result of the correlation analysis showed that they had a great relation between the soil enzyme activities and siol fertility factors.

对12种不同种植模式的6个土壤酶活性和7个土壤肥力因子进行测定,运用相关分析和典型相关分析方法对数据进行分析,以期阐明沿江丘陵地区土壤酶活性与土壤肥力因子的关系。相关分析的结果表明土壤酶活性与土壤肥力因子密切相关,多数呈极显著正相关。

Results showed that the activity of soil enzymes was obviously different.Among the different vegetation types,the activity of soil enzymes under Tilia mandshurica forests was the highest except peroxidase,whereas that under shrub-grass was the lowest.The activity of soil urease and alkaline phosphate under shrub was higher than that under the mixed forests.Activity of soil catalase and phosphate under Larix principis-rupprechtii forests was higher than that under Pinus tabulaeformis.

结果表明:不同植被类型的土壤酶活性有显著的区别,其中除过氧化物酶外,糠椴林的土壤酶活性均属最高水平,而灌草丛所有酶活性都属最低水平;灌木丛中脲酶和碱性磷酸酶活性显著高于杂木林;华北落叶松林的磷酸酶和过氧化氢酶活性均高于油松林。

The result of GPR investigation in west Jilin shows that the radar waveform of saline-alkali soil is different from that of tillable soil, and this can be used to distinguish tillable soil from saline-alkali soil. The extent of salinization can be determined according to the relativity of spectra.

吉林西部盐碱地区的探地雷达调查表明,盐碱地与耕地土的雷达回波具有明显差别,根据振幅的衰减特征可以精确区分耕地与盐碱地,根据频谱中高频峰值与土壤有机质含量的相关性可定性评价土壤的盐碱化程度。

The content of soil ulmin,and the entire nitrogen have slightly rise; compares to 20 years ago , the average content of soil effective phosphorus has slightly increased,but the condition that the soil lack of the phosphorus is still obviously;Athough the content of fast-acting potassium has slightly down,it still stand in a low level,so the soil can't satisfies the needs of the plant normal live.

土壤有机质、全氮含量略有上升;土壤有效磷平均含量比20年前略增加,但缺磷状况仍十分明显;速效钾含量略有下降,仍处于较低水平,不能满足作物正常生长的需要。

This paper,describes the RIC construction technology and its equipments,introduces construction process and compaction scheme,analyzes parameters of uncompacted fill soil and gravel-soil,compacted fill soil,and abutment backside soil,and reviews detection method.

文中阐述了RIC工法及其设备,介绍了RIC工法施工工艺流程及夯击方案,研究了RIC工法在松散填土和填石工程、补强夯实工程及结构物台背填土夯实工程施工中的施工技术参数控制,并综述了RIC工法的施工检测方法。

Over a 20-year period there was no increase in soil water content in the grazed grassland at depths of 2~9.9 m. There was a small increase(0.5~3.7 mm/a) in soil water content in the protected grassland, however the slow rate of increase suggests that at least 150 years would be needed for ungrazed grassland soils to regain water content similar to that present prior to planting trees. Recharge of deep soil moisture was faster in cropland(15 mm/a), but at this rate it would still take about 40 years to restore cropland soil water content to pre-plantation conditions.

结果表明,人工林死后的放牧荒坡在20a的时间里,其土壤水分没有补偿;人工林死后的保护草地土壤水分有微弱恢复迹象,但年恢复速度在0.5~3.7 mm之间,以这样的速度恢复到持续放牧荒坡的土壤含水量,至少需要150a以上;林后农地土壤含水量有恢复趋势,年平均恢复速度为15 mm左右,其土壤含水量要恢复到持续农地当前的水平,大约需要40a的时间。

Planted forests can deplete deep soil water, forming an obstacle to sustainable land use in the semi-arid area of Loess Plateau. The purpose of this study was to examine effects of grazing and cropping on replenishment of deep soil water where forest plantations had depleted soil moisture at depths of 2~9.9 m. We compared soil moisture on plantation plots with that on plots where plantations were replaced by crops, grazed grassland, and ungrazed grassland seperately.

为了研究黄土丘陵半干旱区人工林迹地土壤水分恢复情况,该文以正在生长的人工林土壤水分含量为人工林迹地土壤水分恢复的起点,并分别以持续农地和持续放牧荒坡的土壤含水量为林后农地和草地土壤水分恢复的上限,对位于黄土丘陵半干旱区绥德县境内的人工林迹地土壤水分恢复情况进行了研究。

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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。

Oh, and I bought myself a new laptop," he said."

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