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1

Johnson, C. B. "Inorganic nitrogen metabolism." Phytochemistry 27, no. 5 (January 1988): 1569. http://dx.doi.org/10.1016/0031-9422(88)80250-4.

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2

Scott, TA. "Inorganic Nitrogen Metabolism." Biochemical Education 16, no. 1 (January 1988): 54. http://dx.doi.org/10.1016/0307-4412(88)90042-8.

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3

Roberts, E. H. "Inorganic nitrogen metabolism." Agricultural Systems 27, no. 4 (January 1988): 318. http://dx.doi.org/10.1016/0308-521x(88)90041-8.

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4

Elmerich, C. "Inorganic nitrogen metabolism." Biochimie 70, no. 8 (August 1988): 1121–22. http://dx.doi.org/10.1016/0300-9084(88)90275-1.

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5

Patel, PD, MV Patel, KC Ombase, KD Mevada, AP Patel, and YC Lakum. "Real Time Nitrogen Management through Organic and Inorganic Sources in Wheat." Journal of Pure and Applied Microbiology 12, no. 2 (June 30, 2018): 1001–10. http://dx.doi.org/10.22207/jpam.12.2.64.

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6

Clay, D. E., C. C. Carlson, P. W. Holman, T. E. Schumacher, and S. A. Clay. "Banding nitrogen fertilizer influence on inorganic nitrogen distribution." Journal of Plant Nutrition 18, no. 2 (February 1995): 331–41. http://dx.doi.org/10.1080/01904169509364905.

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7

Richardson, David J., and Nicholas J. Watmough. "Inorganic nitrogen metabolism in bacteria." Current Opinion in Chemical Biology 3, no. 2 (April 1999): 207–19. http://dx.doi.org/10.1016/s1367-5931(99)80034-9.

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8

Fernandez, E., and A. Galvan. "Inorganic nitrogen assimilation in Chlamydomonas." Journal of Experimental Botany 58, no. 9 (March 9, 2007): 2279–87. http://dx.doi.org/10.1093/jxb/erm106.

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9

Gu, Binhe, and Vera Alexander. "Seasonal variations in dissolved inorganic nitrogen utilization in a subarctic Alaskan lake." Archiv für Hydrobiologie 126, no. 3 (February 2, 1993): 273–88. http://dx.doi.org/10.1127/archiv-hydrobiol/126/1993/273.

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10

Ingendahl, Detlev, Eike Haseborg, Melanie Meier, Olaf Van der Most, Helen Steele, and Dietrich Werner. "Linking hyporheic community respiration and inorganic nitrogen transformations in the River Lahn (Germany)." Fundamental and Applied Limnology 155, no. 1 (December 7, 2002): 99–120. http://dx.doi.org/10.1127/archiv-hydrobiol/155/2002/99.

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11

George, T. Adrian, and Bharat B. Kaul. "Electron transfer in inorganic nitrogen fixation." Inorganic Chemistry 30, no. 5 (March 1991): 882–83. http://dx.doi.org/10.1021/ic00005a004.

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12

Grigal, D. F. "Atmospheric Deposition and Inorganic Nitrogen Flux." Water, Air, & Soil Pollution 223, no. 6 (March 15, 2012): 3565–75. http://dx.doi.org/10.1007/s11270-012-1128-2.

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13

Corredor, Jorge E., and Julio Morell. "Inorganic nitrogen in coral reef sediments." Marine Chemistry 16, no. 4 (July 1985): 379–84. http://dx.doi.org/10.1016/0304-4203(85)90058-1.

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14

Lee, Seul-Bi, Jwa-Kyung Sung, Ye-Jin Lee, Jung-Eun Lim, Yo-Sung Song, Deog-Bae Lee, and Suk-Young Hong. "Analysis of Soil Total Nitrogen and Inorganic Nitrogen Content for Evaluating Nitrogen Dynamics." Korean Journal of Soil Science and Fertilizer 50, no. 2 (April 30, 2017): 100–105. http://dx.doi.org/10.7745/kjssf.2017.50.2.100.

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15

Bergström, Lars F., and Holger Kirchmann. "Leaching of Total Nitrogen from Nitrogen‐15‐Labeled Poultry Manure and Inorganic Nitrogen Fertilizer." Journal of Environmental Quality 28, no. 4 (July 1999): 1283–90. http://dx.doi.org/10.2134/jeq1999.00472425002800040032x.

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16

Smith, M. Scott, Charles W. Rice, and Eldor A. Paul. "Metabolism of Labeled Organic Nitrogen in Soil: Regulation by Inorganic Nitrogen." Soil Science Society of America Journal 53, no. 3 (May 1989): 768–73. http://dx.doi.org/10.2136/sssaj1989.03615995005300030023x.

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17

Sainju, Upendra M., Zachary N. Senwo, Ermson Z. Nyakatawa, Irenus A. Tazisong, and K. Chandra Reddy. "Poultry Litter Application Increases Nitrogen Cycling Compared with Inorganic Nitrogen Fertilization." Agronomy Journal 102, no. 3 (May 2010): 917–25. http://dx.doi.org/10.2134/agronj2009.0482.

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18

Middelburg, J. J., and J. Nieuwenhuize. "Nitrogen Isotope Tracing of Dissolved Inorganic Nitrogen Behaviour in Tidal Estuaries." Estuarine, Coastal and Shelf Science 53, no. 3 (September 2001): 385–91. http://dx.doi.org/10.1006/ecss.2001.0805.

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19

Müller, S., and K. Beer. "The relationships between soil inorganic nitrogen levels and nitrogen fertilizer requirements." Agriculture, Ecosystems & Environment 17, no. 3-4 (September 1986): 199–211. http://dx.doi.org/10.1016/0167-8809(86)90043-5.

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20

Kunza, Lisa A., and Robert O. Hall. "Nitrogen fixation can exceed inorganic nitrogen uptake fluxes in oligotrophic streams." Biogeochemistry 121, no. 3 (August 19, 2014): 537–49. http://dx.doi.org/10.1007/s10533-014-0021-z.

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21

Järvinen, Risto. "Nitrogen in the effluent of the pulp and paper industry." Water Science and Technology 35, no. 2-3 (February 1, 1997): 139–45. http://dx.doi.org/10.2166/wst.1997.0502.

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Nitrogen concentrations of effluent before and after treatment plant in two mills have been measured during five days time in a bleached kraft pulp mill and in a newsprint mill. In effluents before treatment the concentration of inorganic nitrogen was low but in the effluent of kraft pulping process, the main part is inorganic nitrogen. In effluent after treatment the concentration of inorganic nitrogen is low. After activated sludge treatment plant the concentration of dissolved organic nitrogen is about 0.6 mg/l and nitrogen in suspended solids determines fluctuation of nitrogen content in treated effluent. There is no need for biological nitrogen removal processes if the addition of nitrogen in the treatment is correct.
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22

Stanley, Emily H., and Amelia K. Ward. "Inorganic Nitrogen Regimes in an Alabama Wetland." Journal of the North American Benthological Society 16, no. 4 (December 1997): 820–32. http://dx.doi.org/10.2307/1468174.

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23

Lee, David J., Daniel C. Bowman, D. Keith Cassel, Charles H. Peacock, and Thomas W. Rufty. "Soil Inorganic Nitrogen under Fertilized Bermudagrass Turf." Crop Science 43, no. 1 (2003): 247. http://dx.doi.org/10.2135/cropsci2003.0247.

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24

Lee, David J., Daniel C. Bowman, D. Keith Cassel, Charles H. Peacock, and Thomas W. Rufty. "Soil Inorganic Nitrogen under Fertilized Bermudagrass Turf." Crop Science 43, no. 1 (2003): 247. http://dx.doi.org/10.2135/cropsci2003.2470.

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25

Turpin, David H., Greg C. Vanlerberghe, Alan M. Amory, and Robert D. Guy. "The inorganic carbon requirements for nitrogen assimilation." Canadian Journal of Botany 69, no. 5 (May 1, 1991): 1139–45. http://dx.doi.org/10.1139/b91-146.

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In the green alga Selenastrum minutum (Naeg.) Collins the assimilation of NH4+ into the full suite of protein amino acids requires at least three separate and distinct inorganic carbon fixing reactions, catalyzed by the enzymes ribulose 1,5-bisphosphate carboxylase/oxygenase (Rubisco), phosphoenolpyruvate carboxylase (PEPC), and carbamoyl phosphate synthetase. In this paper we examine the requirements for CO2 fixation of NH4+ assimilation in this organism. When grown under N-sufficient conditions, NH4+ assimilation is directly dependent upon photosynthetic CO2 fixation to provide carbon skeletons for amino acid synthesis. When cultured under N-limited conditions, the cells accumulate starch, which is then available for amino acid synthesis. This alleviates the requirement of photosynthetic CO2 fixation for NH4+ assimilation. N-limited cells, however, still exhibit a nonphotosynthetic CO2 requirement for N assimilation that is mediated through PEPC. This activity of PEPC increases during N assimilation to replenish TCA cycle intermediates consumed during amino acid synthesis. The in vivo activity of this enzyme is tightly regulated so that there are ~0.3 moles C fixed per mole N assimilated. In S. minutum PEPC is regulated primarily by the ratio of glutamine/glutamate, thus providing a mechanism by which primary NH4+ assimilation modulates the supply of carbon for amino acid biosynthesis. Activation of PEPC during NH4+ assimilation occurs in both the light and the dark. Key words: dissolved inorganic carbon, nitrogen assimilation, phosphoenolpyruvate carboxylase, photosynthesis, amino acid synthesis, respiration.
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26

Woo, Dong K., and Praveen Kumar. "Mean age distribution of inorganic soil-nitrogen." Water Resources Research 52, no. 7 (July 2016): 5516–36. http://dx.doi.org/10.1002/2015wr017799.

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27

Erler, Dirk V., Isaac R. Santos, and Bradley D. Eyre. "Inorganic nitrogen transformations within permeable carbonate sands." Continental Shelf Research 77 (April 2014): 69–80. http://dx.doi.org/10.1016/j.csr.2014.02.002.

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28

HU, CHENG, SHUANG-LAI LI, YAN QIAO, DONG-HAI LIU, and YUN-FENG CHEN. "EFFECTS OF 30 YEARS REPEATED FERTILIZER APPLICATIONS ON SOIL PROPERTIES, MICROBES AND CROP YIELDS IN RICE–WHEAT CROPPING SYSTEMS." Experimental Agriculture 51, no. 3 (November 18, 2014): 355–69. http://dx.doi.org/10.1017/s0014479714000350.

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SUMMARYLong-term fertilization experiment has been conducted since 1981 to study the effect of soil management practices on soil fertility, soil carbon and nitrogen sequestration, soil culturable microbe counts and crop yields at the Nanhu Experimental Station in the Hubei Academy of Agricultural Sciences (situated in the middle reach of the Yangtze River and the rice–wheat cropping system). The experiment was designed with the following eight treatments: (1) unfertilized treatment: Control; (2) inorganic nitrogen fertilizer treatment: N; (3) inorganic nitrogen plus inorganic phosphorus fertilizer treatment: NP; (4) inorganic nitrogen, inorganic phosphorus plus inorganic potassium fertilizer treatment: NPK; (5) pig dung compost (manure) treatment: M; (6) inorganic nitrogen fertilizer plus manure: NM; (7) inorganic nitrogen, inorganic phosphorus fertilizer plus manure treatment: NPM and (8) inorganic nitrogen, inorganic phosphorus, inorganic potassium fertilizer plus manure treatment: NPKM. The results showed that long-term application of organic manure in combination with inorganic fertilizer significantly (p < 0.05) increased soil organic C concentrations compared with the corresponding inorganic fertilizers alone. Soil organic C contents were significantly (p < 0.05) increased in balanced application of NPK fertilizers in comparison to unbalanced application of fertilizers. After 30 years of experiment, soil organic C and total N sequestration rate averagely were 0.48 t ha−1 year−1 and 28.3 kg ha−1 year−1 in the fertilized treatments respectively; nevertheless, it were 0.27 t ha−1 year−1 and 9.7 kg ha−1 year−1 in the unfertilized treatment. Application of organic fertilizer in combination with inorganic fertilizer significantly (p < 0.05) increased culturable microbial counts compared with the corresponding inorganic fertilizers alone. The balanced application of NPK fertilizers significantly (p < 0.05) increased culturable microbial counts compared with unbalanced application of fertilizers. The average grain yield of wheat and rice was significantly (p < 0.05) higher in organic manure combined with inorganic fertilizer treatment than in inorganic fertilizer alone and unfertilized control. Therefore, long-term application of organic manure combined with inorganic fertilizer and balanced application of NPK fertilizers could increase soil organic C and total N sequestration, culturable microbial counts and crop grain yields.
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29

Kim, Haryun. "Review of inorganic nitrogen transformations and effect of global climate change on inorganic nitrogen cycling in ocean ecosystems." Ocean Science Journal 51, no. 2 (June 2016): 159–67. http://dx.doi.org/10.1007/s12601-016-0014-z.

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30

Metcalfe, R. J., J. Nault, and B. J. Hawkins. "Adaptations to nitrogen form: comparing inorganic nitrogen and amino acid availability and uptake by four temperate forest plants." Canadian Journal of Forest Research 41, no. 8 (August 2011): 1626–37. http://dx.doi.org/10.1139/x11-090.

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There are few examinations of the relative availability and plant uptake of inorganic N and amino acid N in temperate forest regions. We determined the availability of amino acid N and inorganic N in soils under two shrub species ( Vaccinium ovalifolium Sm. versus Rubus spectabilis Pursh) on three sites near Jordan River, British Columbia, over a growing season. We compared biomass production of the two shrubs and two conifers ( Picea sitchensis (Bong.) Carr. and Pseudotsuga menziesii (Mirb.) Franco var. menziesii) when given inorganic N (20:80 or 80:20 NH4+–NO3–) or organic N (glycine and glutamic acid) and assessed short-term uptake (24 h) of 15N-labelled NH4+, NO3–, glycine, or glutamic acid by the four species. Water-extracted soil concentrations of NH4+ were up to 1.5 times greater than NO3– averaged across sites. Concentrations of amino acid N and inorganic N were similar on soils under Rubus , but the amino acid N to inorganic N ratio was up to 2.4:1 in soils under Vaccinium . Soils dominated by Rubus had up to twice the NO3–-N and two thirds the amino acid N concentrations of soils dominated by Vaccinium, averaged across sites and Rubus had relatively high short-term 15NO3– uptake. The dry biomass of conifers was approximately four times greater when supplied mainly with NH4+ compared with NO3–, but biomass of the two shrub species was similar in both inorganic N treatments. All plants had comparable rates of short-term 15N uptake from amino acids and inorganic N, suggesting that amino acids could contribute to the N nutrition of these temperate species; however, dry biomass of all four species grown with amino acids was less than one half that of plants grown with inorganic N.
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31

Cosby, B. J., R. C. Ferrier, A. Jenkins, B. A. Emmett, R. F. Wright, and A. Tietema. "Modelling the ecosystem effects of nitrogen deposition: Model of Ecosystem Retention and Loss of Inorganic Nitrogen (MERLIN." Hydrology and Earth System Sciences 1, no. 1 (March 31, 1997): 137–58. http://dx.doi.org/10.5194/hess-1-137-1997.

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Abstract. A catchment-scale mass-balance model of linked carbon and nitrogen cycling in ecosystems has been developed for simulating leaching losses of inorganic nitrogen. The model (MERLIN) considers linked biotic and abiotic processes affecting the cycling and storage of nitrogen. The model is aggregated in space and time and contains compartments intended to be observable and/or interpretable at the plot or catchment scale. The structure of the model includes the inorganic soil, a plant compartment and two soil organic compartments. Fluxes in and out of the ecosystem and between compartments are regulated by atmospheric deposition, hydrological discharge, plant uptake, litter production, wood production, microbial immobilization, mineralization, nitrification, and denitrification. Nitrogen fluxes are controlled by carbon productivity, the C:N ratios of organic compartments and inorganic nitrogen in soil solution. Inputs required are: 1) temporal sequences of carbon fluxes and pools- 2) time series of hydrological discharge through the soils, 3) historical and current external sources of inorganic nitrogen; 4) current amounts of nitrogen in the plant and soil organic compartments; 5) constants specifying the nitrogen uptake and immobilization characteristics of the plant and soil organic compartments; and 6) soil characteristics such as depth, porosity, bulk density, and anion/cation exchange constants. Outputs include: 1) concentrations and fluxes of NO3 and NH4 in soil solution and runoff; 2) total nitrogen contents of the organic and inorganic compartments; 3) C:N ratios of the aggregated plant and soil organic compartments; and 4) rates of nitrogen uptake and immobilization and nitrogen mineralization. The behaviour of the model is assessed for a combination of land-use change and nitrogen deposition scenarios in a series of speculative simulations. The results of the simulations are in broad agreement with observed and hypothesized behaviour of nitrogen dynamics in growing forests receiving nitrogen deposition.
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32

HU, Guo-Ping, Jing CAO, Hai-Xing YANG, and Hong-Xia WEI. "Coupling effect of inorganic nitrogen and cabbage waste on soil nitrogen mineralization." Chinese Journal of Eco-Agriculture 20, no. 6 (December 6, 2012): 739–45. http://dx.doi.org/10.3724/sp.j.1011.2012.00739.

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33

WIDMER, P., P. BROOKES, and L. PARRY. "Microbial biomass nitrogen measurements in soils containing large amounts of inorganic nitrogen." Soil Biology and Biochemistry 21, no. 6 (1989): 865–67. http://dx.doi.org/10.1016/0038-0717(89)90183-1.

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34

Lindau, C. W., R. D. Delaune, W. H. Patrick, and E. N. Lambremont. "Assessment of stable nitrogen isotopes in fingerprinting surface water inorganic nitrogen sources." Water, Air, and Soil Pollution 48, no. 3-4 (December 1989): 489–96. http://dx.doi.org/10.1007/bf00283346.

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35

Chaffin, Justin D., and Thomas B. Bridgeman. "Organic and inorganic nitrogen utilization by nitrogen-stressed cyanobacteria during bloom conditions." Journal of Applied Phycology 26, no. 1 (September 5, 2013): 299–309. http://dx.doi.org/10.1007/s10811-013-0118-0.

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36

Zebarth, B. J., S. Freyman, and C. G. Kowalenko. "Influence of nitrogen fertilization on cabbage yield, head nitrogen content and extractable soil inorganic nitrogen at harvest." Canadian Journal of Plant Science 71, no. 4 (October 1, 1991): 1275–80. http://dx.doi.org/10.4141/cjps91-178.

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Cabbage (Brassica oleracea L.) was fertilized at rates of 0, 100, 200, 300, 400 and 500 kg N ha−1. Yield and plant total N increased with increasing N rate. Apparent recovery of fertilizer N in the cabbage heads averaged 32% and was independent of N rate. Soil extractable inorganic N at harvest was low and increased with increasing N rate in only one of the 2 yr. Key words: Brassica oleracea, N recovery
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37

Pombeiro, Armando J. L. "Nitrogen ligands." Dalton Transactions 48, no. 37 (2019): 13904–6. http://dx.doi.org/10.1039/c9dt90195g.

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38

Sun, Ying, and Qian Yang. "Research on the Transformation of Nitrogen during Hydrothermal Carbonization of Sludge." MATEC Web of Conferences 175 (2018): 01019. http://dx.doi.org/10.1051/matecconf/201817501019.

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The nitrogen in the sludge mainly exists in the form of inorganic nitrogen and organic nitrogen.In this paper, the transformation of nitrogen during the hydrothermal carbonization of sludge was studied.The results showed that during the hydrothermal carbonization of the sludge, both the total nitrogen and theinorganic nitrogen in hydrochar decrease with the increase of the carbonization temperature. The reason isthat part of the inorganic nitrogen compounds in the sludge undergoes thermal decomposition to releaseNH3, and some organic nitrogen will be hydrolyzed to produce ammonia nitrogen into the liquid phase.
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39

Bray, Robert C. "The inorganic biochemistry of molybdoenzymes." Quarterly Reviews of Biophysics 21, no. 3 (August 1988): 299–329. http://dx.doi.org/10.1017/s0033583500004479.

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Molybednum-containing enzymes (Coughlan, 1980; Spiro, 1985) occupy a significant place in the development of the field now termed inorganic biochemistry. The importance of the metal as a biological trace element depends on its involvement in the known, and perhaps other as yet unknown, molybdoenzymes. That it plays a role in biological nitrogen fixation, the process whereby the enzyme nitrogenase in the root nodules of plants converts atmospheric nitrogen into ammonia, was recognized in the 1930s. The metal is also a constituent of a variety of other enzymes, having first been found in a mammalian enzyme, xanthine oxidase, in the 1950s.
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40

Snapp, S. S., and A. M. Fortuna. "Predicting Nitrogen Availability in Irrigated Potato Systems." HortTechnology 13, no. 4 (January 2003): 598–604. http://dx.doi.org/10.21273/horttech.13.4.0598.

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Growers lack practical decision aides that accurately predict nitrogen (N) credits for organic sources to adjust fertilizer rates. The simulation model, DSSAT, was used to predict N supply in relationship to N demand in irrigated potatoes (Solanum tuberosum). Tuber yield and soil inorganic N levels were substantially higher in the simulations than in field experiment observations, indicating the need for model improvement. DSSAT was successful at predicting relative mineralization rates and potato N uptake for different organic and inorganic N source combinations. Interestingly, both simulation and field experiment observations indicated that combining a high quality organic manure at 5000 lb/acre (5604.2 kg·ha-1), total applied N 250 lb/acre (280.2 kg·ha-1), and a fertilizer source of N 160 lb/acre (179.3 kg·ha-1) markedly increased yields and lowered leaching potential. Simulated tuber yield for the combined treatment was 660 cwt/acre (74.0 t·ha-1) with 48 lb/acre (53.8 kg·ha-1) inorganic-N in the profile at harvest, whereas the highest simulated N fertilizer response was to 235 lb/acre (263.4 kg.·ha-1), which produced 610 cwt/acre (68.4 t·ha-1) with 77 lb/acre (86.3 kg·ha-1) inorganic-N in the profile at harvest. The synchrony of N release and uptake for combined manure and fertilizer treatments may explain the efficient N uptake observed. Common soil types and weather scenarios in Michigan were simulated and indigenous soil N mineralization was predicted to be 6 lb/acre (6.7 kg·ha-1) inorganic-N in the topsoil at planting, similar to observed levels. The increasing aeration associated with a sandy versus a sandy loam soil only slightly increased the predicted rate of mineralization from organic inputs. Simulated soil inorganic N levels with different organic inputs was modestly increased in a warm spring [4.5 °F (2.50 °C) over normal temperatures] compared to a cool spring (-4.5 °F less than normal temperatures). For Michigan irrigated potato systems, DSSAT simulations indicate that the most important factor determining inorganic N supply will be the quality and quantity of organic inputs, not environmental conditions.
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41

Junjie, Zhao, Shou Youping, Bai Jing, and Wang Ning. "Tendency and Causes Analysis of Marine Water Quality of Jinzhou Bay." E3S Web of Conferences 206 (2020): 03003. http://dx.doi.org/10.1051/e3sconf/202020603003.

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Based on the two monitoring data of Jinzhou Bay in July 2008, September 2013 and September 2016, this article analysis the temporal trends of marine water quality of Jinzhou Bay. The average concentration of COD, inorganic nitrogen and phosphate is between 1.09mg/L~1.45mg/L, 0.42mg/L~0.711mg/L and 0.006mg/L~0.03mg/L, respectively. The concentration of inorganic nitrogen showed a downward trend while the concentration of phosphate showed an increased trend. Meanwhile, the concentration of COD had no significant change. Results showed that the inorganic nitrogen concentration and phosphate concentration have good correlation with eutrophication index and Eutrophication parameters(E)showing a clear upward trend. The emission of active phosphates and inorganic nitrogen from land-based pollutants are the main cause of this phenomenon.
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42

Kismányoky, T., and I. Ragasits. "Effects of organic and inorganic fertilization on wheat quality." Acta Agronomica Hungarica 51, no. 1 (April 1, 2003): 47–52. http://dx.doi.org/10.1556/aagr.51.2003.1.6.

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The influence of organic and nitrogen fertilization on the amount and quality of wheat yield was examined in Keszthely on Ramann's brown forest soil containing an average level of potassium, a low level of phosphorus and a medium level of nitrogen. The experiment involved treatments with 0-200 kg/hectare of nitrogen, 100 kg/hectare each of phosphorus (P2O5) and potassium (K2O), farmyard manure, straw and green manure, together with a non-fertilized control. Nitrogen fertilization had a substantial effect on the yield (the 1.98 t/hectare yield was increased threefold by 200 kg/hectare of nitrogen). The treatments modified the quality of wheat significantly. Nitrogen fertilization together with farmyard manure increased the gluten content (to 35.8% compared to 11.35% in the control). The farinographic index increased to 77.4 (from 33.9 in the control) and the Zeleny number also increased significantly (from 10 in the control to 35.5). When low rates of nitrogen were applied overall improvement was not achieved in spite of the favourable influence of farmyard manure.
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43

Zanzotti, Roberto, and Enzo Mescalchin. "Green manure effects on inorganic nitrogen dynamics in soil and its accumulation in grape must." BIO Web of Conferences 13 (2019): 04010. http://dx.doi.org/10.1051/bioconf/20191304010.

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The adoption of green manure practices in organic agriculture is increasingly spreading. This work aims to prove whether winter green manure—when compared to a traditional mineral fertilizer— alters the dynamics of inorganic nitrogen (NO3− and NH4+) availability in soil and the yeast assimilable nitrogen (YAN) in grape musts. During a two-year period, the soil nitrogen content was influenced by climatic trend and, especially, by rainfall. In fact, rainy periods reduced inorganic nitrogen availability in the soil. In both years, the green manure plot presented higher soil content of inorganic nitrogen at fruit-set, while different dynamics were shown over the following phenological phases. The must YAN concentration did not differ among treatments over the two-year experiment.
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44

Scudlark, Joseph R., and Thomas M. Church. "Atmospheric Input of Inorganic Nitrogen to Delaware Bay." Estuaries 16, no. 4 (December 1993): 747. http://dx.doi.org/10.2307/1352433.

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45

Ashworth, Amanda J., Pat D. Keyser, Fred L. Allen, Donald D. Tyler, Adam M. Taylor, and Charles P. West. "Displacing Inorganic Nitrogen in Lignocellulosic Feedstock Production Systems." Agronomy Journal 108, no. 1 (January 2016): 109–16. http://dx.doi.org/10.2134/agronj15.0033.

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46

Banger, Kamaljit, Emerson D. Nafziger, Junming Wang, and Cameron M. Pittelkow. "Modeling Inorganic Soil Nitrogen Status in Maize Agroecosystems." Soil Science Society of America Journal 83, no. 5 (September 2019): 1564–74. http://dx.doi.org/10.2136/sssaj2019.05.0140.

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Chivers, Tristam, and Frank Edelmann. "Transition-metal complexes of inorganic sulphur-nitrogen ligands." Polyhedron 5, no. 11 (1986): 1661–99. http://dx.doi.org/10.1016/s0277-5387(00)84846-9.

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Alexandre, Ana, Dimos Georgiou, and Rui Santos. "Inorganic nitrogen acquisition by the tropical seagrassHalophila stipulacea." Marine Ecology 35, no. 3 (February 25, 2014): 387–94. http://dx.doi.org/10.1111/maec.12128.

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Crouse, K. K., J. J. Varco, and W. F. Jones. "Evaluation of methods for soil inorganic nitrogen analysis." Communications in Soil Science and Plant Analysis 25, no. 3-4 (February 1994): 419–33. http://dx.doi.org/10.1080/00103629409369048.

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50

Crawford, Nigel M., and Brian G. Forde. "Molecular and Developmental Biology of Inorganic Nitrogen Nutrition." Arabidopsis Book 1 (January 2002): e0011. http://dx.doi.org/10.1199/tab.0011.

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