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首页> 外文期刊>Soil & Tillage Research >Long-term management impacts on soil C, N and physical fertility: Part I: Broadbalk experiment
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Long-term management impacts on soil C, N and physical fertility: Part I: Broadbalk experiment

机译:长期管理对土壤碳,氮和物理肥力的影响:第一部分:Broadbalk实验

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摘要

For many centuries manure application to the soil has been common practice. Organic amendments and fertiliser applications can increase crop yields and soil organic matter (SOM). However, the long-term impacts on soil physical fertility are often neglected. This study was carried out on the Broadbalk Wheat Experiment at Rothamsted, UK, established in 1843 on an Aquic/Typic Paleudalf soil. Application of farmyard manure (FYM), N fertiliser and wheat straw on total organic C (CT), labile C (CL) and non-labile C (CNL), total N (NT), mean weight diameter (MWD) and unsaturated hydraulic conductivity (Kunsat) were studied on wheat (Triticum aestivum) and adjacent woodland and pasture areas. Manure additions, N fertiliser and straw incorporation increasedall C fractions, particularly the CL fraction. The addition of 35 t ha-1 year-1 of FYM increased CT to 2.5 times that of the control (no fertiliser) treatment and CL to 5 times that of the control. With highest N application and straw returned, CT increased by 1.3 times and CL by 1.5 times that of the control treatment. There were linear relationships between rate of N fertiliser applied and all C fractions, with the rate of increase almost double with straw than straw removed. Manure application improved MWD, as did high N fertiliser additions with straw returned. Application of N fertiliser only increased MWD and Kunsat (at 10 mm tension) if straw was returned, while the addition of manure resulted in decreased Kunsat. The highest Kunsat rate was onthe high N fertiliser, straw returned treatments. The uncropped areas all had high soil structural stability. Similar relationships occurred between all C fractions and NT and MWD for the high C soils, but relationships were much stronger with CL than the other C fractions in the low C soils. These results showed that soils with low C concentration are more reliant on CL for structural stability.
机译:几个世纪以来,将肥料施用到土壤上一直是惯例。有机改良剂和肥料的施用可以提高作物产量和土壤有机质(SOM)。但是,对土壤物理肥力的长期影响常常被忽略。这项研究是在1843年在英国Rothamsted的Aquac / Typic Paleudalf土壤上进行的Broadbalk小麦实验上进行的。农田肥料(FYM),氮肥和麦秸在总有机碳(CT),不稳定碳(CL)和非不稳定碳(CNL),总氮(NT),平均重量直径(MWD)和非饱和水力中的应用在小麦(Triticum aestivum)以及邻近的林地和牧场上研究了电导率(Kunsat)。粪肥的添加,氮肥和秸秆的掺入增加了所有碳的比例,特别是CL的比例。 FYM 35 t ha-1 year-1的添加使CT增至对照(无肥料)处理的2.5倍,CL增至对照的5倍。施氮量最高,秸秆还田,与对照相比,CT升高了1.3倍,CL升高了1.5倍。氮肥施用量与所有碳元素含量之间存在线性关系,秸秆增加量几乎是秸秆去除量的两倍。粪肥的施用改善了MWD,秸秆还田还增加了高氮肥的施用。如果返回秸秆,施用氮肥只会增加MWD和Kunsat(在10 mm张力下),而添加肥料会导致Kunsat减少。 Kunsat率最高的是高氮肥,秸秆还田。未耕种地区均具有较高的土壤结构稳定性。对于高碳土壤,所有碳组分与NT和MWD之间都存在相似的关系,但与CL的关系要比低碳土壤中的其他碳组分强得多。这些结果表明,低C浓度的土壤在结构稳定性上更依赖CL。

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