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温度和改良剂对澳大利亚部分土壤中氮矿化的影响。

Effects of temperature and amendments on nitrogen mineralization in selected Australian soils.

作者信息

Thangarajan Ramya, Bolan Nanthi S, Naidu Ravi, Surapaneni Aravind

机构信息

Centre for Environmental Risk Assessment and Remediation, University of South Australia, Mawson Lakes, SA, 5095, Australia.

出版信息

Environ Sci Pollut Res Int. 2015 Jun;22(12):8843-54. doi: 10.1007/s11356-013-2191-y. Epub 2013 Oct 11.

Abstract

The effects of temperature (18, 24, and 37 °C) and form of nitrogen (N) input from various sources (organic-green waste compost, biosolids, and chicken manure; inorganic-urea) on N transformation in three different Australian soils with varying pH (4.30, 7.09, and 9.15) were examined. Ammonification rate (ammonium concentration) increased with increase in temperature in all soil types. The effect of temperature on nitrification rate (nitrate concentration) followed 24 > 37 > 18 °C. Nitrification rate was higher in neutral and alkaline soils than acidic soil. Mineral N (bioavailable N) concentration was high in urea treatments than in organic N source treatments in all soil types. Acidic soil lacked nitrification activity resulting in low nitrate (NO3) buildup in urea treatment, whereas a significant NO3 buildup was noticed in green waste compost treatment. In neutral and alkaline soils, the nitrification activity was low at 37 °C in urea treatment but with a significant NO3 buildup in organic amendment added soils. Addition of organic N sources supplied ammonia oxidizing bacteria thereby triggering nitrification in the soils (even at 37 °C). This study posits the following implications: (1) inorganic fertilizer accumulate high NO3 content in soils in a short period of incubation, thereby becoming a potential source of NO3 leaching; (2) organic N sources can serve as possible source of nitrifying bacteria, thereby increasing bioavailable N (NO3) in soils regardless of the soil properties and temperature.

摘要

研究了温度(18、24和37°C)以及来自不同来源的氮(N)输入形式(有机——绿色废物堆肥、生物固体和鸡粪;无机——尿素)对三种不同pH值(4.30、7.09和9.15)的澳大利亚土壤中氮转化的影响。在所有土壤类型中,氨化率(铵浓度)均随温度升高而增加。温度对硝化率(硝酸盐浓度)的影响顺序为24 > 37 > 18°C。中性和碱性土壤中的硝化率高于酸性土壤。在所有土壤类型中,尿素处理中的矿质氮(生物可利用氮)浓度高于有机氮源处理。酸性土壤缺乏硝化活性,导致尿素处理中硝酸盐(NO3)积累量低,而在绿色废物堆肥处理中则观察到显著的NO3积累。在中性和碱性土壤中,尿素处理在37°C时硝化活性较低,但在添加有机改良剂的土壤中有显著的NO3积累。添加有机氮源提供了氨氧化细菌,从而引发了土壤中的硝化作用(即使在37°C时)。本研究提出以下几点启示:(1)无机肥料在短时间培养中会在土壤中积累高含量的NO3,从而成为NO3淋失的潜在来源;(2)有机氮源可作为硝化细菌的可能来源,从而增加土壤中的生物可利用氮(NO3),而不受土壤性质和温度的影响。

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