简介：基于前辈的研究，并且对比与水水平和一个好含水土层的系统的水温度反应特征装载的应力的模式，这份报纸在装载的应力的三个模式引起的一口井在水温度回答的机制上得出一个初步的结论，即煤气的逃跑，为装载的有弹性的震波应力加热分散和冷水穿入机制；为装载的震波应力的破裂渗出物机制和为长时期的压力消散的热机制减缓在地震准备阶段装载的应力。这份报纸为装载的应力的每个模式说明典型观察例子并且在他们的机制上做初步的研究。

简介：FinemeasurementshavebeenconductedtotemperaturesandtheirgradientsofsixwellsoftheJinshaRiverGroundwaterObservationalNetwork.Theresultsshowthattheinfluencedepthsofsunradiationheatare50mto125m,averagetemperaturegradientsinthewellsrangefrom0.11to2.81℃/hmandmostare1～2℃/hm,andthetemperaturegradientsonvarieddepthsectionsofonewellarehighlychangeable.Lithologyofstrataandtheirintegrity,particularlyhigh-anglecrashedfaultzones,haveimposedmajoreffectsontheinfluencedepthsofsunradiationheatandtemperaturegradientsofthewells.Themicrodynamiccharacteristicsofwatertemperature,suchascoseismiceffects,tidaleffectsandanomaliesofthewellspriortoearthquakes,probablydepend,toalargedegree,onthetemperaturegradientsofthedepthsatwhichthewatertemperaturesensorsaresettled.

简介：

简介：Heatflowisinevitablyaccompaniedbytemperaturechange,thus,thewatertemperaturecoseismicresponseduringearthquakeactivityshouldalsoobeythelawsofthermodynamics.TakingtheMS8.0Wenchuan,Sichuan,ChinaearthquakeandtheM9.0Tohoku,Japanearthquakeasanexample,andbasedonthedataofwatertemperaturecoseismicresponsesobservedinwellZK26inHaikou,HainanProvince,China,weinvestigatetherelationshipbetweenwellwatertemperaturechangeandheattransferinthecoseismicresponseprocessandtherelevantthermodynamicmechanismbyusingthenumericalsimulationmethodforthermodynamicequations.Then,throughforwardmodeling,weobtainseveralsimulationcurvesofwatertemperaturechangeinresponsetoearthquakesalongthewelldepthatdifferenttimes.Thesimulatedcurvesofwatertemperaturechangeapproximatelyfittheobservedcurves.Consequently,basedonthevariationoftemperature,wefindthatthemodesofwellwatertemperaturecoseismicresponse(ascending,descendingorstable)arerelatedtofactorssuchasthelocationofsensors,distributionandlocationofheatsources,thespanbetweensensorsandheatsources.

简介：Inordertodeterminethedegreeofreturning-to-zerooftemperaturesofdeformedcalcite,aseriesofrock-breakingexperimentsweredesignedtotestcalcite-richlimestonesamplesunderfixedconfiningpressuresanddifferenttemperatures.Theconsolidateddeformedsamplesintheirinitialstatewereobservedunderamicroscopeandthemicroscopicindicatorsindifferentzero-returningstateswereputforward,thusprovidingamicroscopicfoundationforevaluationofreliabilityofdatingvaluesofdeformationincalcite.Atlast,thecorrectionofdatingvaluesofdeformationforsampleswhosetemperaturehasnotyetreturnedtozeroisdiscussed.

简介：在到地震预言的MODIS卫星遥感数据的应用程序的学习，论文第一次提出一个量的方法与反常亮度温度(BT)为象素估计比率为云移动的增加和一个初步的计划。原则是第一，无云的数据在时间，但是在不同的天内的一样的时期由一样的卫星观察了(通常1天到3天)是mosaiced得到晴朗天空的高比率，然后BT变化曲线和每个象素的mcan平方差别(MSD)从盖住的区域与数据被计算每天决定今日的BT数据作为标准用两倍MSD在某个象素由是正常的。为有反常BT增加的象素的比率能被与整个区域的全部的象素划分反常象素的全部的数字计算。在台湾区域的一系列最近的地震上的分析证明为有反常BT增加的象素的比率，通常在零附近波动，有突然的改进1天到在媒介强壮的地震前的20天。为识别地震预兆的一个新方法能被从MODIS卫星遥感随反常BT增加为象素分析比率的变化与经常的地震活动在区域通过特殊研究发现，这被期望红外线(红外)云的效果从被移开的信息到某个程度。