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首页> 外文期刊>European Journal of Soil Science >Impact of biochar addition on water retention, nitrification and carbon dioxide evolution from two sandy loam soils.
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Impact of biochar addition on water retention, nitrification and carbon dioxide evolution from two sandy loam soils.

机译:生物炭添加对两种砂壤土土壤保水,硝化和二氧化碳释放的影响。

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摘要

Some intensive agricultural practices result in soil degradation through loss of soil organic matter. Organic farming may mitigate this problem, if managed properly, but may result in a yield penalty compared with conventional systems. Biochar addition to soil could influence both agricultural systems, but previous studies are not definitive about its impact on soil processes. Sandy soils are more susceptible to the effects of reduced soil organic matter on soil hydrology and nutrient dynamics. Nitrogen (N) is important for crop growth and soil water content can influence its transformation and cycling. This study explored the effect of biochar amendment on soil water retention and nitrification processes in soils under organic and conventional management. Carbon dioxide evolution was used as an indicator of related microbial activity. A water release curve study and a 60-day incubation experiment were set up to consider the effect of biochar application on organically and conventionally managed sandy loam soils. The results showed that addition of biochar increased water retention for both soils and this is attributed to its porous structure. On incubation of an organically managed soil, with green-waste compost, initial ammonium level was small, reflecting microbial demand for N. The large cation exchange capacity of the organically managed soil retained ammonium, reducing availability for nitrification. Carbon dioxide evolution increased with continuing small contents of ammonium and nitrate when biochar was added to the organically managed soil. Biochar enhanced nitrification without increased respiration during incubation of a conventionally managed soil with added mineral N; a possible explanation for this enhancement is the increase in pH resulting from the biochar addition.
机译:一些集约化农业实践导致土壤有机质流失,导致土壤退化。如果管理得当,有机耕作可以缓解这个问题,但是与常规系统相比,有机耕作可能会导致产量下降。土壤中添加生物炭可能会影响两个农业系统,但先前的研究尚不确定其对土壤过程的影响。沙质土壤更容易受到土壤有机质减少对土壤水文学和养分动力学的影响。氮(N)对作物生长很重要,土壤水分会影响其转化和循环。这项研究探讨了生物炭改良剂在有机和常规管理下对土壤保水和硝化过程的影响。二氧化碳的释放被用作相关微生物活性的指标。建立了放水曲线研究和60天的温育实验,以考虑生物炭施用对有机和常规处理的沙壤土的影响。结果表明,生物炭的添加增加了两种土壤的保水性,这归因于其多孔结构。在将有机管理的土壤与绿色废物堆肥一起孵育时,初始铵含量很小,反映了微生物对氮的需求。有机管理的土壤具有较大的阳离子交换能力,可以保留铵,从而降低了硝化作用。当将生物炭添加到有机管理的土壤中时,随着氨和硝酸盐含量的不断降低,二氧化碳的释放增加。在常规处理的土壤中添加矿物质氮的过程中,生物炭可增强硝化作用,而不会增加呼吸作用;这种增强的可能解释是由于添加生物炭导致pH值增加。

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