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Field- and watershed-scale evaluation of water quality trends due to changes in landscape and management practices.

机译:由于景观和管理方式的变化,对水质趋势进行实地和流域尺度评估。

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Large N losses from the Upper Mississippi River Basin contributing to hypoxia in the Gulf of Mexico are due to high concentrations of nitrate-N and large tile drain discharges from row crop agriculture. A water quality simulation model was calibrated and validated at the field and watershed scales for tile drainage and associated nitrate-N losses in the Seven Mile Creek watershed of Nicollet County under various scenarios. The first series of simulations involved N fertilizer rate and timing. At the field scale, reductions in N fertilizer rate (from 176 to 121 kg/ha) resulted in a 14% reduction in nitrate-N losses, while at the watershed scale reducing N fertilizer rate (from 179 to 112 kg/ha) resulted in a 23% reduction in nitrate-N losses. Shifting N fertilizer application from fall to spring produced a 5.5% reduction in nitrate-N losses at the field scale (N rate 121 kg/ha), while a similar shift at the watershed scale produced a 12% reduction (N rate 112 kg/ha). A series of long-term simulations (1955-2004) were performed at the watershed scale to investigate impacts of changes in climate, cropping systems, N fertilizer rates, area of wetlands and tile drain spacing. Using constant 2003 baseline conditions, nitrate-N losses increased 185% over the last 50 years due to an increasingly wetter climate. Historical records of land use, wetland area, crop rotations, crop yields, N fertilizer application rates and tile drain spacings were then used to investigate nitrate-N losses for 1955, 1967, 1978 and 2003 conditions. When accounting for these changes, but excluding nitrate transformations in wetlands, nitrate losses were 14.5, 19.0, 23.1 and 36.7 kg/ha for the 1955, 1967, 1978, and 2003 periods, respectively. Wetlands covered 15% of the study area in 1955, while none exist at present. Water budgets were calculated considering the direct effects of wetlands 72.6 cm deep, along with changes in area of agricultural land, cropping systems, crop yields, N application rate and tile drain spacing. Discharges were reduced by 29% in 1955 relative to 2003, while nitrate-N losses were reduced by 73% in 1955 relative to 2003.
机译:密西西比河上游流域的大量氮素流失导致了墨西哥湾的缺氧,这是由于硝态氮含量高以及行作农业中大量的瓷砖排水造成的。在各种情况下,对尼科尔雷特县七哩溪流域的瓷砖排水和相关的硝态氮损失进行了实地和流域尺度的水质模拟模型的校准和验证。第一系列模拟涉及氮肥施用量和施肥时间。在田间尺度上,氮肥用量减少(从176公斤/公顷至121公斤/公顷)导致硝酸盐氮损失减少14%,而在分水岭规模上,氮肥用量减少(从179公斤/公顷至112公斤/公顷)使硝酸盐氮损失减少了23%。从秋季到春季,氮肥施用量的变化在田间尺度上减少了5.5%的硝酸盐氮损失(氮比率121千克/公顷),而分水岭尺度上的类似变化导致氮素损失减少了12%(氮比率112千克/公顷)。哈)。在分水岭规模上进行了一系列长期模拟(1955-2004年),以调查气候变化,耕作制度,氮肥用量,湿地面积和瓷砖排水沟间距的影响。在2003年不变的基准条件下,由于气候越来越潮湿,过去50年中硝酸盐氮的损失增加了185%。然后,利用土地利用,湿地面积,作物轮作,作物产量,氮肥施用量和瓷砖排水沟间距的历史记录来调查1955年,1967年,1978年和2003年的硝态氮损失。如果考虑到这些变化,但不包括湿地中的硝酸盐转化,则1955年,1967年,1978年和2003年的硝酸盐损失分别为14.5、19.0、23.1和36.7 kg / ha。 1955年,湿地覆盖了研究区域的15%,而目前尚不存在。计算水预算时要考虑到72.6厘米深的湿地的直接影响,以及耕地面积,耕作制度,作物产量,氮肥施用量和瓷砖排水沟间距的变化。 1955年的排放量相对于2003年减少了29%,而硝酸盐氮的损失相对于2003年减少了73%。

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