干旱区盐渍地景观危险度评价方法——以新疆渭干河-库车河流域为例

土壤的盐渍化是干旱区农业发展的主要障碍,也是影响绿洲生态环境稳定的重要因素。利用破碎度(C)、分离度(F)、优势度(D)等景观格局指数及景观脆弱度(S)建立了盐渍化景观危险度(SR)评价指数以研究渭干河-库车河流域盐渍化地的危险程度。选择新疆渭干河-库车河流域1989年和2001年Landsat-TM图像为本底数据,结合野外调查样本进行实例验证。研究表明,在12年期间,由于研究区内人类活动不断加强,景观结构变化导致盐渍化景观危险度指数明显增高,综合盐渍化危险度指数(SCR)由0.4832上升到0.5234,盐渍化危险度有扩大的趋势,评价结果与实际情况有较好的一致性。该方法对提高不同干旱区域土壤盐渍地危险度评价的准确性及定量化具有一定的参考意义。     

磷酸三(1,3-二氯-2-丙基)酯导致小鼠神经毒性结局的潜在靶点研究

磷酸三(1,3-二氯-2-丙基)酯(TDCPP)在环境介质及生物样本中被广泛检出,为探究TDCPP的潜在神经毒性以及作用机制,以C57BL/6小鼠为动物模型,考察经300 mg·kg-1·d-1的TDCPP持续染毒35 d后,小鼠大脑皮层神经功能相关因子及血清代谢组学的变化.结果显示,小鼠在TDCPP染毒35 d后,大...     

Earthquake risk reduction: An examination of local regulatory efforts

We develop an understanding of local governmental efforts to address earthquake risks. Our data for a sample of California and Washington cities' risk-reduction efforts sort into two different clusters of leading jurisdictions as contrasted with a cluster of lagging jurisdictions. We explain differences among the three categories of cities in terms of different political-economic factors. Local governmental willingness and ability to undertake risk-reduction programs have more to do with local political demands and community resources than with objective risk or previous earthquake experience. State mandates have a selective impact on local risk-reduction efforts. The principal policy lessons concern the need to address gaps in local risk-reduction efforts through more careful targeting of federal and state earthquake programs and by including stronger teeth within state mandates.     

Riparian buffers and potentially unstable ground

The spatial coincidence between riparian buffers of various widths and extents and potentially unstable ground was quantified using a physically based model for shallow landslide initiation and GIS for two watersheds on the Olympic Peninsula, Washington, USA. The proportion of the potentially unstable ground in each watershed within riparian buffers is a function of both buffer width and the extent of the stream channel network being buffered. While current buffers required by Washington State cover less than 5% of the potentially unstable ground, buffering all stream channels in these watersheds with 100-m buffers covered 75%–90% of the potentially unstable areas. Our analyses further show that: (1) riparian buffers are not efficient mechanisms for protecting potentially unstable ground, and (2) identifying potentially unstable ground using a physically based model should prove more effective for designing methods to reduce shallow landsliding hazards than relying on extensive buffer zones along stream channels.