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1)  soil temperature
土温
1.
Interactive heat transfer of air and soil temperature in greenhouse;
温室内气温与土温相关性传热模型
2.
The effect of soil temperature on the growth was studied in Rudbeckia hirta, a biennial herbaceous flower.
这些说明适宜的土壤温度使根系的吸收活力增强,有利于植物地上部的生长发育,同时植物根系会通过功能补偿作用对不良土温做出适应性反应,以减少不良土温对植物的危害。
3.
Based on the latest achievements in meteorology,the heating effect in the ground - atmosphere system discussed, and the mechanism of heating and cooling of the soil and the air analyzed,the traditional relationship about solar radiation,air temperature and soil temperature is revised and developed, and a new relationship is put forward.
依据气象学的最新研究成果,探讨了地—气系统的热力效应,分析了土壤及大气的增热与冷却机理,对传统理论中关于太阳辐射、气温和土温的关系进行了修正和拓展,提出了它们之间的相关关系。
2)  soil temperature
土壤温度
1.
The effects of soil temperature and moisture of artificial ecological restoration under different rocky desertification degrees in karst region—A case study of the Huajiang gorge area,Guizhou;
喀斯特地区不同等级石漠化人工生态恢复的土壤温度及水分效应——以贵州省花江峡谷为例
2.
Eftect of green grassland on soil temperature;
草坪绿地对土壤温度的调节作用
3.
Effects of water content variation on soil temperature process and water exchange;
含水量变化对土壤温度和水分交换的影响研究
3)  Greenhouse soil
温室土壤
1.
The effects of ozone treatment on greenhouse soil chemical properties and melon yield;
臭氧对温室土壤化学性质和甜瓜产量的影响
2.
Effects of moisture, temperature and nitrogen supply rate on NO_3~-N accumulation in greenhouse soil;
温室土壤硝态氮积累的温度、水分、施氮量耦合效应
3.
Coupling effects of temperature,moisture,and nitrogen application on greenhouse soil pH and EC
温度、水分和施氮量对温室土壤pH及电导率的耦合作用
4)  H(?) Tenperature Mud Acid
高温土酸
5)  ground temperature
土壤温度
1.
The resuming course of ground temperature of source heat pump is simulatively researched after the ground temperature heat pump is performed for some time.
应用数值方法对土壤源热泵运行一段时间后土壤温度的恢复过程进行了研究。
2.
The analysis based on the daily maximum, minimum and daily range of the ground temperature at different depths at D110 site, northern part of Tibetan Plateau, showed that from surface to 40cm depth the variation of the daily maximum ground temperature was strong.
通过藏北高原D110点一年中不同深度土壤温度的日最高值、日最低值及日温差的分析,表明从0cm~40cm,土壤温度的日最高值的变化剧烈,而日最低值的变化则相对平稳。
3.
Based on the ground temperature data at different sites in the Northern Tibetan Plateau obtained during the GAME_Tibet field observation, the features of the latitude effect and elevation effect of the ground temperature in the Northern Tibetan Plateau were analyzed.
利用GAME- Tibet 野外观测期间所得藏北高原不同地点土壤温度资料, 对藏北高原土壤温度分布纬向地带性和垂直地带性特征进行分析, 结果表明夏季土壤温度分布主要表现为高度效应,而冬季土壤温度分布主要表现为纬度效应。
6)  warm frozen soil
高温冻土
1.
Because there are defects such as fracture and cavity in the warm frozen soil,and their distributions are random,the elastic moduli and strengths are still uncertain;and they will be stochastic variables submitted to one of probability distribution,even if the temperature of frozen soil is the same.
由于高温冻土内部裂隙、空洞等缺陷分布有很大的随机性,即使在同一土温下,其弹性模量及强度不是某一确定值,而是服从某一概率分布规律的随机变量。
2.
Based on the characteristics of random distribution of defects such as fissure and void in warm frozen soil,a stochastic damage model for warm frozen soil under uniaxial compression is developed by using continuous damage theory and probability and statistic theory.
从高温冻土内部裂隙、空洞等缺陷的随机分布出发,基于连续损伤理论和概率与数理统计理论,建立了高温冻土的单轴随机损伤本构模型,并利用3种不同试验温度下的实测数据与之对比分析。
补充资料:土温
1.土壤的温度。
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