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61.
Agricultural use of soils implies tillage and often compaction and therefore influences processes on soil surface and affects infiltration of water into the subsoil. Although many studies on soil surface processes or flow patterns in soils exist, works relating both are rare in literature. We did two tracer experiments with Brilliant Blue FCF on a tilled and compacted plot and a non‐tilled one to investigate water storage on the soil surface during simulated rainfall and changes of soil microtopography, to analyse the associated flow patterns in the soil and to relate both to tillage and compaction. Our results show that storage was larger on the tilled and compacted plot than on the non‐tilled one. After tillage, transport processes above the plough pan were partly disconnected from those underneath because macropores were disrupted and buried by the tillage operation. However, preferential flow along cracks occurred on both plots and the macropores buried below the tillage pan still functioned as preferential flow paths. Therefore, we conclude that the studied soil is susceptible to deep vertical solute propagation at dry conditions when cracks are open, irrespective of tillage and compaction. Copyright © 2012 John Wiley & Sons, Ltd. 相似文献
62.
《地学前缘(英文版)》2022,13(2):101324
The causes of the global mass extinction that occurred around the Permian–Triassic boundary have been widely studied through the geological record and in various locations. The results show that volcanic activity was a key factor in initiating the crisis during the Late Permian. Compared to other thermal events triggered by volcanic activity, pyrolysis of petroleum in Pre-Permian reservoirs has rarely been suggested as a significant source of the greenhouse gases that caused the mass extinction. In this study, geochemical analysis is carried out of a huge paleo-oil reservoir in the Yangtze Block (YB), South China. The detection of mineral inclusions and pyrobitumens is evidence of rapid pyrolysis of accumulated oil in the Ediacaran reservoir. New evidence from hydrothermal minerals and the presence of domain mesophase in the pyrobitumen suggest that the pyrolysis process occurred abruptly and that greenhouse gases were rapidly released through venting pipes. The dating of such a complex geological event in this old and deeply buried reservoir is inevitably difficult and potentially unreliable. However, cross-validation of the multiple evidence sources, including hydrothermal minerals and domain mesophase, indicates that the rapid oil pyrolysis must have been driven by a major thermal event. Reconstruction of burial and thermal histories suggests that the thermal event was most likely to have been triggered by the Emeishan Large Igneous Province (ELIP), which was in a period of significant volcanic activity during the Late Permian. Massive volumes of gases, including methane, carbon dioxide, and possibly hydrogen sulfide, were released, causing a significant increase in greenhouse gases that may have contributed to global warming and the resulting mass extinction during the Late Permian Crisis (LPC). 相似文献
63.
Summary The geology and structure of the Mexico Basin are discussed and hypotheses developed to explain the magnification of wave amplitudes during the 1985 earthquake. 相似文献
64.
Alessio Nicosia Costanza Di Stefano Vincenzo Palmeri Vincenzo Pampalone Vito Ferro 《水文研究》2021,35(10):e14407
Flow velocity is one of the most important hydrodynamic variables for both channelized (rill and gullies) and interrill erosive phenomena. The dye tracer technique to measure surface flow velocity Vs is based on the measurement of the travel time of a tracer needed to cover a known distance. The measured Vs must be corrected to obtain the mean flow velocity V using a factor αv = V/Vs which is generally empirically deduced. The Vs measurement can be influenced by the method applied to time the travel of the dye-tracer and αv can vary in different flow conditions. Experiments were performed by a fixed bed small flume simulating a rill channel for two roughness conditions (sieved soil, gravel). The comparison between a chronometer-based (CB) and video-based (VB) technique to measure Vs was carried out. For each slope-discharge combination, 20 measurements of Vs, characterized by a sample mean Vm, were carried out. For both techniques, the frequency distributions of Vs/Vm resulted independent of slope and discharge. For a given technique, all measurements resulted normally distributed, with a mean equal to one, and featured by a low variability. Therefore, Vm was considered representative of surface flow velocity. Regardless of roughness, the Vm values obtained by the two techniques were very close and characterized by a good measurement precision. The developed analysis on αv highlighted that it is not correlated with Reynolds number for turbulent flow regime. Moreover, αv is correlated neither with the Froude number nor with channel slope. However, the analysis of the empirical frequency distributions of the correction factor demonstrated a slope effect. For each technique (CB, VB)-roughness (soil, gravel) combination, a constant correction factor was statistically representative even if resulted in less accurate V estimations compared to those yielded by the slope-specific correction factor. 相似文献
65.
新建拉林铁路桑珠岭隧道高地应力、高地温隧道开挖过程中岩爆灾害突出。考虑开挖卸荷与温降共同耦合作用,对隧道开挖过程中不同温度时洞周应力释放过程进行数值模拟,同时对隧道开挖后的二次应力进行现场实测,就高地温对隧道洞周应力的影响进行了比较分析,最后就不同岩爆判据下高地温对岩爆发生的影响性进行了讨论。研究结果表明,采用应力释放率和温降指标反映开挖卸荷与温降共同耦合作用能合理描述高地应力高地温段开挖过程中的应力特征和岩爆发生规律。当温降超过55 ℃,应力释放率大于40%以后, 及 量值随应力释放率增大而线性增长,当应力释放率达到100%时达到最大,不同位置洞周应力拱脚处增长最快,拱顶次之,其他位置较低。在开挖中受高地温影响岩爆发生时间提前,岩爆发生等级亦不断增加。 相似文献
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68.
底泥释磷及其对杭州西湖富营养化的影响 总被引:35,自引:7,他引:28
杭州西湖是一个小型浅水湖泊,底泥由上部藻骸腐泥和下部泥炭层构成,其显著特点是有机碳含量特别高,氮含量也相当高,而磷的富集程度相对较低。通过实验室和现场模拟研究,考察了pH值、温度、溶解氧、氧化还原电位及上覆水种类等环境因素对底泥释磷量和释磷速率的影响。上覆水pH值在6.5—7.0范围内底泥释磷量最低;在较高或较低pH值时,释磷量倍增。升高水温或降低上覆水溶解氧浓度均能加速释磷。实验室模拟西湖底泥最大释磷量为0.368μgP/g。夏季现场模拟平均释磷速率为1.02mg P/m~2·d;由此估算底泥释磷量达1.346tP/a,相当于年平均外部入湖磷负荷的36.4%。底泥释磷对西湖富营养化起着不容忽视的影响。 相似文献
69.
20世纪80年代以来,浙江近海的主要渔业资源呈现衰退趋势,因此从2000年至今相关单位持续开展人工增殖放流以修复渔业资源。文章基于2017—2021年浙江近海鱼类增殖放流统计数据作出分析,对比放流资金、放流数量、放流物种等变化趋势得出:2017—2021年主要在浙江近海12处重要的增殖放流海域投放了大黄鱼(Larimichthys crocea)、黑鲷(Acanthopagrus schlegelii)、黄姑鱼(Nibea albiflora)、条石鲷(Oplegnathus fasciatus)等16种海洋鱼类,累计投入放流资金11 285.9万元,投放海洋鱼类苗种共计46 799.8万尾,其中标志鱼投入共330.1万元,放流苗种48.8万尾。调查和文献报道显示,增殖放流对增加浙江近海海洋鱼类生物资源量、恢复海洋鱼类群落结构、保护海洋生物多样性,促进海洋渔业的发展等方面起到积极的作用。根据调研情况和相关文献梳理了增殖放流存在的问题并提出了相关的改进建议,以期为今后科学规范实施增殖放流提供参考。 相似文献
70.
Tolo Harbour has received massive discharges of municipal sewage, agricultural wastes and cottage industrial effluents, via three river systems, in the past two decades before the mid Eighties. The Harbour is almost land locked and poorly flushed. The soft sediment acted as a sink for nutrients and organic pollutants. After a decade of efforts in establishing and enforcing water pollution control legislations and upgrading wastewater treatment facilities, the sediments have turned into sources of nutrients and exert a measurable oxygen demand upon the overlying waters. In vitro measurements showed that the sediments oxygen demand (SOD) was between 17.6 and 54.3 mgo2 · m-2 · h-1. The maximum rates of release of ortho-phosphate phosphorus and ammonia nitrogen were 15.0 and 206.0 mg · m-2 · h-1, respectively. 相似文献