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Nitrogen biogeochemistry of aquaculture pond sediments.

机译:养殖池塘沉积物的氮生物地球化学。

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摘要

Aquaculture pond water quality is dominated by planktonic processes, although the high surface-to-volume ratio suggests that sediment has the potential to effect important changes in water quality. The objectives of this research were to evaluate annual variation of sediment nitrogen biogeochemistry and develop a model of annual variation in ammonia concentration in a commercial channel catfish pond. In addition, the effects of physical and chemical sediment management techniques on water quality in aquatic mesocosms were evaluated.; Sediment nitrogen was dominated by organic (92-96%) and adsorbed ammonium (2-4%) fractions. Porewater ammonium comprised the smallest yet most dynamic component of sediment N, with maximum concentrations measured during summer. Porewater ammonium concentrations were 4-20x higher than in the water column. Sediments were sinks for oxygen and oxidized nitrogen and sources of carbon dioxide and ammonium. Molecular diffusion accounted for only 1.4-14.9% of ammonium flux suggesting that mineralization of organic matter at the sediment surface was rapid. Denitrification rates were limited by low ambient oxidized nitrogen concentrations, although denitrification potential was substantial.; A simulation model accurately described annual variation of catfish pond ammonium concentration. Ammonium production was partitioned between fish excretion (67-75%) and sediment diffusion (25-33%). Phytoplankton ammonium uptake exceeded nitrification during the growing season (April-October); nitrification was a more important removal mechanism than phytoplankton uptake during the winter (November-March). Model output was most sensitive to changes in the partition of nitrogenous excretion, average feeding rate, and the phytoplankton specific uptake rate.; Sediment disturbance in organically-enriched aquatic mesocosms improved water quality for fish production. Dissolved oxygen concentration was higher and ammonia concentration was lower in mesocosms stocked with fish. Whole-tank respiration was inversely related to sediment disturbance. Nitrification associated with suspended particles was inversely related to C:N ratio of organic inputs.; Nitrate enrichment of aquatic mesocosms did not improve water quality for fish production. Elevated concentrations of ammonia and nitrite were associated with high dissimilatory nitrate reduction rates. Substantial quantities of organic matter mineralization mediated by nitrate were inferred from alkalinity accumulation. Dissolved oxygen concentrations were increased and soluble phosphorus concentrations were decreased only slightly as a function of nitrate enrichment.
机译:水产养殖池塘的水质主要由浮游过程控制,尽管高的表积比表明沉积物有可能影响水质的重要变化。这项研究的目的是评估沉积物氮生物地球化学的年变化,并开发商业化channel鱼池塘氨浓度的年变化模型。此外,还评估了理化沉积物管理技术对水生介体水质的影响。沉积物氮主要由有机(92-96%)和吸附的铵(2-4%)组成。孔隙水铵构成了沉积物N最小但最具活力的组成部分,夏季测得的最大浓度。孔隙水中的铵浓度比水柱高4-20倍。沉积物是氧气和氧化氮的汇,以及二氧化碳和铵的来源。分子扩散仅占铵通量的1.4-14.9%,这表明沉积物表面有机物的矿化作用很快。尽管反硝化潜力很大,但反硝化率受到环境氧化氮浓度低的限制。模拟模型准确地描述了fish鱼池塘铵盐浓度的年度变化。铵的生产在鱼排泄物(67-75%)和沉积物扩散(25-33%)之间分配。在生长季节(4- 10月),浮游植物的铵盐吸收超过硝化作用。在冬季(11月至3月),硝化作用比浮游植物的吸收更为重要。模型输出对氮排泄物的分配,平均摄食率和浮游植物比吸收率的变化最敏感。富含有机物的水生介体中的泥沙扰动改善了鱼类生产的水质。鱼类放养的介体中溶解氧浓度较高,氨浓度较低。全罐呼吸与沉积物扰动成反比。与悬浮颗粒相关的硝化作用与有机投入物的碳氮比成反比。水生介体的硝酸盐富集并未改善鱼类生产的水质。氨和亚硝酸盐浓度升高与硝酸盐异化率高相关。硝酸盐介导的大量有机物矿化是从碱度积累中推断出来的。溶解氧的浓度增加,而可溶性磷的浓度仅随着硝酸盐富集的增加而略有降低。

著录项

  • 作者

    Hargreaves, John Albert.;

  • 作者单位

    Louisiana State University and Agricultural & Mechanical College.;

  • 授予单位 Louisiana State University and Agricultural & Mechanical College.;
  • 学科 Biology Limnology.; Biogeochemistry.; Agriculture Animal Culture and Nutrition.; Agriculture Fisheries and Aquaculture.
  • 学位 Ph.D.
  • 年度 1995
  • 页码 242 p.
  • 总页数 242
  • 原文格式 PDF
  • 正文语种 eng
  • 中图分类 生物地球化学、气体地球化学;饲料;水产、渔业;
  • 关键词

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