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21.
22.
The majority of emissions of nitrous oxide – a potent greenhouse gas (GHG) – are from agricultural sources, particularly nitrogen fertilizer applications. A growing focus on these emission sources has led to the development in the United States of GHG offset protocols that could enable payment to farmers for reducing fertilizer use or implementing other nitrogen management strategies. Despite the development of several protocols, the current regional scope is narrow, adoption by farmers is low, and policy implementation of protocols has a significant time lag. Here we utilize existing research and policy structures to propose an ‘umbrella’ approach for nitrogen management GHG emissions protocols that has the potential to streamline the policy implementation and acceptance of such protocols. We suggest that the umbrella protocol could set forth standard definitions common across multiple protocol options, and then modules could be further developed as scientific evidence advances. Modules could be developed for specific crops, regions, and practices. We identify a policy process that could facilitate this development in concert with emerging scientific research and conclude by acknowledging potential benefits and limitations of the approach.

Key policy insights

  • Agricultural greenhouse gas market options are growing, but are still underutilized

  • Streamlining protocol development through an umbrella process could enable quicker development of protocols across new crops, regions, and practices

  • Effective protocol development must not compromise best available science and should follow a rigorous pathway to ensure appropriate implementation

  相似文献   
23.
Equations have been presented previously which predict that reflector curvature can affect significantly seismic reflection amplitudes at both zero and nonzero source-receiver offsets. Here the fact that faults are generally concave-upward is used to examine the curvature effect for compaction-driven faults which the sediments have both exponential and logarithmic porosity decreases with increasing depth.The curvature effect is generally larger over upwardly concave reflectors where amplitudes can either increase with offset (exposed focus) or decrease with offset (buried focus). The magnitude of the effect depends on the ratio between the depth to the structure and the radius of curvature of the structure. A phase change of 90° also occurs at a critical offset in the case of an exposed focus concave-upward reflector, with decreasing amplitude at offsets larger than the critical value. Dip move-out (DMO) dominantly removes the amplitude variation with offset due to curvature. These results suggest that when looking for amplitude variations with offset in a fault prospect, DMO should be applied as a preprocessing step. Compaction-driven faults have an exposed focus and, for an exponential variation of porosity with depth, there is a maximum curvature effect at a depth roughly the same as the scaling depth for the porosity. Logarithmic porosity with depth variations suggest a continued increase in the curvature effect of faults with increasing depth, to a maximum amplitude increase of about 35% relative to a plane interface.  相似文献   
24.
设计城市地貌图应注重城市地貌在建城区、边缘区和城市经济辐射区范围内的区域分异规律。编制城市地貌图应遵循:环境功能,应用性,突出重点和图面协调三个原则。据此编制了成都市1:6500建城区,1:5万边缘区和1:20万城市经济辐射区三种城市地貌图。  相似文献   
25.
航空像片在活断层研究中的应用   总被引:2,自引:1,他引:2       下载免费PDF全文
江娃利 《地震地质》1991,13(4):323-331
航片判读活断层的依据是断层地形学。航片判读活断层的关键是找出变位地形。变位地形是指由构造作用形成,非自然侵蚀作用所能形成的地形。航片判读变位地形的可信度分为三类。垂河向陡坎、背河向陡坎及反坡向陡坎被认为是可信度工的第四纪活动的变位地形。判读走滑断层的变位方向及变位量,需注意地貌面上的线性地物。利用不同变位基准的不同变位量可判读断层活动期次。本文通过中日航片判读活断层的14个实例,对变位地形的识别予以说明  相似文献   
26.
温纳偏置电测深法压制表层电性不均匀体影响的研究   总被引:4,自引:1,他引:4  
巷道底板浮煤等电性不均匀体及厚度变化是造成煤矿井下电测深曲线畸变的主要因素。通过模型实验研究了温纳偏置电测保法压制浮煤等表层电性不均匀体影响的能力。用感度分析法讨论了表层电性不均匀体产生地电干扰的机制。实测结果表明,该方法改善了电测深曲线质量,有效地提高了电测深法地质应用效果。  相似文献   
27.
利用2003年小江流域的TM影像,结合实地调查,再根据流域地质分布和地貌发育情况,将流域地貌类型划分为岩溶地貌和非岩溶地貌两个一级类型景观,在此基础上,根据地貌发育程度结合高程情况,将岩溶区又划分为6个岩溶景观,非岩溶地貌分为两个二级类型景观。应用景观生态学原理,并通过Fragstats 3.3软件在流域尺度上计算了一些相关指标。结果表明:岩溶区的景观生态特征总体上体现了其生态环境的特殊性和脆弱性,地表水资源溃乏,土层薄、土壤资源零星分布且易流失,造成未利用地面积大,石漠化现象严重,土地利用程度低的特点。非岩溶区景观生态由于耕地和林地占绝对优势,石漠化面积少,香农多样性指数和均匀度低,景观的异质性较低,结构较为简单。  相似文献   
28.
The paper introduces the steps and methods of multi-approach,multi-level exploration of buried faults in thick Quaternary sediment regions by taking the test exploration of the Yinchuan active fault as example.Based on the comprehensive analyses of previous data,we choose the Xinqushao Village of Xingqing District of Yinchuan City as the test site for the comprehensive exploration.Firstly,we adopted shallow seismic investigation with group intervals of 10m,5m and 1m to gradually trace layer by layer the master fault of the Yinchuan buried fault from a deep depth to a shallow depth where drilling could be used.Then,with composite geological profile drilling,we determined the precise location and dip angle of the fault.The drilling show the buried depth of the upper offset point is 8.3m.Finally,large-scale trenching revealed that the actual buried depth of the upper offset point of the fault is 1.5m from the ground surface and there are paleoearthquake events of 5 stages.Combined with the preliminary result of corresponding sample age,we conclude the Yinchuan buried fault is a mid to late Holocene active fault.  相似文献   
29.
The damage distribution in Adra town (south‐eastern Spain) during the 1993 and 1994 Adra earthquakes (5.0 magnitude), that reached a maximum intensity degree of VII (European Macroseismic Scale (EMS scale)), was concentrated mainly in the south‐east zone of the town and the most relevant damage occurred in reinforced concrete (RC) buildings with four or five storeys. In order to evaluate the influence of ground condition on RC building behaviour, geological, geomorphological and geophysical surveys were carried out, and a detailed map of ground surface structure was obtained. Short‐period microtremor observations were performed in 160 sites on a 100m × 100m dimension grid and Nakamura's method was applied in order to determine a distribution map of soil predominant periods. Shorter predominant periods (0.1–0.3 s) were found in mountainous and neighbouring zones and larger periods (greater than 0.5 s) in thicker Holocene alluvial fans. A relationship T = (0.049 ± 0.001)N, where T is the natural period of swaying motion and N is the number of storeys, has been empirically obtained by using microtremor measurements at the top of 38 RC buildings (ranging from 2 to 9 storeys). 1‐D simulation of strong motion on different soil conditions and for several typical RC buildings were computed, using the acceleration record in Adra town of the 1993 earthquake. It is noteworthy that all the aforementioned results show the influence of site effects in the degree and distribution of observed building damage. Copyright © 2007 John Wiley & Sons, Ltd.  相似文献   
30.
复杂地质构造波动方程数值模拟   总被引:3,自引:2,他引:3  
利用全声波方程进行地震波场的数值模拟,虽然可以计算全声波波场值,但是也常常会出现层间多次波,给资料解释造成一定的困难。作者在本文中根据无反射声波方程,采用有限差分数值解法,实现了自激自收时间剖面的制作,避免了层间多次波的产生。本方法不但允许速度有纵向变化,而且允许速度有横向变化,这使得模拟复杂地质构造的地震响应成为可能。实际计算结果表明,该方法是一种行之有效的自激自收时间剖面的计算机数值模拟方法。  相似文献   
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