The groundwater level represents a critical factor to evaluate hillside landslides. A monitoring system upon the real-time
prediction platform with online analytical functions is important to forecast the groundwater level due to instantaneously
monitored data when the heavy precipitation raises the groundwater level under the hillslope and causes instability. This
study is to design the backend of an environmental monitoring system with efficient algorithms for machine learning and knowledge
bank for the groundwater level fluctuation prediction. A Web-based platform upon the model-view controller-based architecture
is established with technology of Web services and engineering data warehouse to support online analytical process and feedback
risk assessment parameters for real-time prediction. The proposed system incorporates models of hydrological computation,
machine learning, Web services, and online prediction to satisfy varieties of risk assessment requirements and approaches
of hazard prevention. The rainfall data monitored from the potential landslide area at Lu-Shan, Nantou and Li-Shan, Taichung,
in Taiwan, are applied to examine the system design. 相似文献
Hg emission flux from various land covers, such as forests, wetlands, and urban areas, have been investigated. China has the largest area of coalfield in the world, but data of Hg flux of coalfields, especially, those with coal fires, are seriously limited. In this study, Hg fluxes of a coalfield were measured using the dynamic flux chamber (DFC) method, coupled with a Lumex multifunctional Hg analyzer RA-915+ (Lumex Ltd., Russia). The results show that the Hg flux in Wuda coalfield ranged from 4 to 318 ng m?2 h?1, and the average value for different areas varied, e.g., coal-fire area 99 and 177 ng m?2 h?1; no coal-fire area 19 and 32 ng m?2 h?1; and backfilling area 53 ng m?2 h?1. Hg continued to be emitted from an underground coal seam, even if there were no phenomena, such as vents, cracks, and smog, of coal fire on the soil surface. This phenomenon occurred in all area types, i.e., coal-fire area, no coal-fire area, and backfilling area, which is universal in Wuda coalfield. Considering that many coalfields in northern China are similar to Wuda coalfield, they may be large sources of atmospheric Hg. The correlations of Hg emission flux with influence factors, such as sunlight intensity, soil surface temperature, and atmospheric Hg content, were also investigated for Wuda coalfield.