首页> 外文期刊>Transactions of the ASABE >RIPARIAN ECOSYSTEM MANAGEMENT MODEL (REMM): II. TESTING OF THE WATER QUALITY AND NUTRIENT CYCLING COMPONENT FOR A COASTAL PLAIN RIPARIAN SYSTEM
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RIPARIAN ECOSYSTEM MANAGEMENT MODEL (REMM): II. TESTING OF THE WATER QUALITY AND NUTRIENT CYCLING COMPONENT FOR A COASTAL PLAIN RIPARIAN SYSTEM

机译:RIPARIAN生态系统管理模型(REMM):II。沿海平原RIPARIAN系统水质和养分循环成分的测试

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摘要

The Riparian Ecosystem Management Model (REMM) was used to simulate nitrogen (N), phosphorus (P), and carbon (C) cycling and transport in a Coastal Plain riparian buffer system near Tifton, Georgia. The riparian buffer consisted of zone 3 (grass next to a row crop field); zone 2 (mature pine forest downslope from zone 3); and zone 1 (hardwood forest downslope from zone 2, adjacent to a stream). Uncalibrated simulation results for a five-year period were compared to measured values for the same time period at the research site. In general, simulated water table nutrient concentrations were within one standard deviation of observed values on an annual basis. Surface runoff loads exiting zone 3 for most N and P forms were simulated within one standard deviation of the observed. In contrast zone 2, surface runoff loads for inorganic N species were an order of magnitude lower than observed. Although some of the surface runoff differences (observed vs. simulated) were large in relative terms, the overall trends within the riparian buffer were generally well-represented and differences were not large in absolute terms. Simulated values for one of the most important processes responsible for effectiveness of riparian zones — denitrification, were within the range of those observed. Much of the temporal dynamics of the observed data were also captured in the REMM simulations. Certain constraints of the model use are discussed, but REMM appears to be useful for representing many of the specific processes and general trends in riparian ecosystem buffers.
机译:河岸生态系统管理模型(REMM)用于模拟佐治亚州蒂夫顿附近的沿海平原河岸缓冲系统中氮(N),磷(P)和碳(C)的循环和运输。河岸缓冲区由3区(行耕田旁边的草丛)组成。 2区(3区成熟的松树林下坡);和区域1(区域2的硬木森林下坡,与溪流相邻)。将五年期间的未经校准的模拟结果与研究地点同期的测量值进行比较。通常,模拟的地下水位养分浓度每年都在观测值的一个标准偏差之内。对于大多数N和P形式,离开区域3的地表径流负荷在观测值的一个标准偏差内进行了模拟。在对比区2中,无机N物质的表面径流负荷比观察到的低一个数量级。尽管一些地表径流差异(相对于模拟而言)比较大,但沿河缓冲带内的总体趋势通常可以很好地表示,绝对值差异也不大。导致河岸带有效性的最重要过程之一(反硝化)的模拟值在所观察到的范围内。在REMM模拟中还捕获了许多观测数据的时间动态。讨论了模型使用的某些限制条件,但是REMM对于表示河岸生态系统缓冲区中的许多特定过程和一般趋势似乎很有用。

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