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81.
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通过利用一个较为完善的大气环流模式(GCM)进行了一系列青藏高原不断隆升的数值模拟试验结果.共进行了11个改变地形高度的数值试验,即对欧亚大陆上现代大地形所在地区(约10～60°N,50～140°E)陆地上所有格点的地形高度分别取为现代地形高度值的100%,90%,80%,70%,…,10%,外加一个无地形试验MOO,共完成了11个试验.结合与干旱化有关的地质记录,探讨了高原隆起在欧亚内陆及北非干旱演化过程中的作用.结果表明,仅仅改变高原地区地形高度的数值试验结果与气候变化地质记录在趋势上有可比性,青藏高原隆升是中亚及北非地区在地质时间尺度上干旱化加剧的重要原因,但却不是上述干旱区形成的根本原因. 相似文献
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84.
Olivier Gourgue Richard ComblenJonathan Lambrechts Tuomas KärnäVincent Legat Eric Deleersnijder 《Advances in water resources》2009
We present a flux-limiting wetting–drying approach for finite-element discretizations of the shallow-water equations using discontinuous linear elements for the elevation. The key ingredient of the method is the use of limiters for generalized nodal fluxes. This method is implemented into the Second-generation Louvain-la-Neuve Ice-ocean Model (SLIM), and is verified against standard test cases. The method is further applied to the wetting and drying of sand banks in the Scheldt Estuary, which is located in northern Belgium and the southern Netherlands. The results obtained for both the benchmarks and the realistic problem illustrate the accuracy of the method in describing the hydrodynamics in the vicinity of dry areas. In particular, the method strictly conserves mass, and there is no transport through dry areas. 相似文献
85.
The ability of psammophyte(a plant that grows in sand or sandy soil) to withstand and recover from severe droughts is crucial for desertification control and restoration of degraded vegetation in semi-arid sandy land in northern China.Responses of the photo-synthetic gas exchange and chlorophyll fluorescence of an annual(Setaria viridis) were measured through three cycles of soil drying and rewatering.Results showed that the net photosynthesis rate(Pn) decreased by 95 percent,91 percent,and 61 percent at end of three drought periods;the stomatal conductance(gs) decreased by 72 percent,73 percent,and 53 percent;the transpiration rate(Tr) decreased by 70 percent,69 percent,and 37 percent;and water-use efficiency(WUE) decreased by 83 percent,69 percent,and 38 percent.At the same time,the trapping probability with no dark adaptation(FV’/FM’) decreased by 70 percent,12 percent,and 10 percent,while the electron transport per cross-section(ET0’/CS’0) decreased by 80 percent,45 percent,and 13 percent.The intercellular CO2(Ci) increased by 1.77,1.02,and 0.66 times,and the dissipation per cross-section(DI0’/CS0’) increased by 98 percent,28 percent,and 22 percent.These results indicated that S.viridis was subjected to photoinhibition and some nonstomatal limitation of photosynthesis under drought.However,the above photosynthetic characteristics were restored to control values after three or four days of rewatering.The capability to recover from drought may contribute to the plant’s use of water as efficiently as possible.Furthermore,during the subsequent drought spells,suppression of Pn,gs,Tr,FV’/FM’,and ET0’/CS0’ decreased or slowed down following the drying and rewatering alternations,especially in the third drought spell. 相似文献
86.
Experimental sandstone weathering using different wetting and drying moisture amplitudes 总被引：1，自引：0，他引：1
Wetting and drying is an acknowledged yet still poorly understood rock weathering process. Previous experiments documented in the literature measure physical changes or mass loss in relation to moisture oscillations but only one study directly compares different moisture amplitudes by using different modes of moisture application. In this experimental study, four sets of sandstone tablets are subjected to 48 h wetting and drying cycles at set moisture content fluctuations of 29, 42, 56 and 63% respectively. A common moisture application, full immersion, is used for all four sets. Mass loss after 52 cycles averaged 0·27%, some three times more than that of the control samples. Average porosity of the samples increased, while water absorption capacities and the saturation coefficients of the samples decreased. No discernable difference in mass loss or change in physical properties was found between the different sample sets. When compared with previous studies, results suggest that the effect of moisture application type may be more of a controlling factor on the weathering effect than actual moisture content achieved. A need to move towards a more standardized approach in wetting and drying experimental studies is emphasized. Copyright © 2007 John Wiley & Sons, Ltd. 相似文献
87.
大直径嵌岩桩残余应变状态分析 总被引：2，自引：0，他引：2
通过对2根大直径嵌岩灌注桩（人工挖孔）加载前应变状态连续监测,初步分析了桩身残余产生的原因、分布规律和对桩受力性状的影响,并得到如下结论：（1）混凝土的干缩是产生残余应变的主要因素;（2）桩身的残余应变随空间和时间变化是有规律的,但诸多施工因素（如爆破,地下水和浇注方式）会使其分布不均匀或弱化桩侧岩石的约束力;（3）桩身局部的残余应变会超过混凝土的极限拉应变而产生裂缝,失去对桩身钢筋的保护能力,并且桩身整体收缩会减小桩端与地基的接触力。以上结论可为工程实践提供参考。 相似文献
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89.
To explore the impact of temperature difference (TD) on the disintegration of redbed softrock, three types of redbed rock, collected from Nanxiong Basin, were analyzed under three different treatments: TD, wetting and drying (WD), and TDWD-temperature difference and WD. To better understand the influence of different ranges of TD on disintegration during WD cycles, pH (hydrogen ion concentration) values, electrical conductivity (EC) values, and concentration of cations in leachate released during treatment were measured. The results show that no significant change can be observed under single TD treatment but that TD can increase the disintegration rate by accelerating the water–rock interaction. The effect of TD is more significant for rock with weak resistance to disintegration. 相似文献
90.