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Effects of fertilizer type and rate on labile soil fractions of a sandy Cambisol—long-term and short-term dynamics

机译:肥料类型和施用量对沙质坎比索尔不稳定土壤组分的影响-长期和短期动态

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The application of density fractionation is an established technique, but studies on short-term dynamics of labile soil fractions are scarce. Objectives were (1) to quantify the long-term and short-term dynamics of soil C and N in light fraction (LFOC, LFON, ρ ≤ 2.0 g cm–3) and microbial biomass C (Cmic) in a sandy Cambisol as affected by 28 y of different fertilization and (2) to determine the incorporation of C4-C into these labile fractions during one growing season of amaranth. The treatments were: straw incorporation plus application of mineral fertilizer (MSI) and application of farmyard manure (FYM) each at high (MSIH, FYMH, 140–150 kg N ha–1 y–1) and low (MSIL, FYML, 50–60 kg N ha–1 y–1) rates at four field replicates. For all three sampling dates in 2008 (March, May, and September), stocks of LFOC, LFON and Cmic decreased in the order FYMH FYML MSIH, MSIL. However, statistical significance varied markedly among the sampling dates, e.g., with LFOC being significantly different (p ≤ 0.05) in the order given above (sampling date in March), significantly different depending on the fertilizer type (May), or nonsignificant (September). The high proportion of LFOC on the stocks of soil organic C (45% to 55%) indicated the low capacity of soil-organic-matter stabilization on mineral surfaces in the sandy Cambisol. The incorporation of C4-C in the LFOC during one growing season of amaranth was small in all four treatments with C4-LFOC ranging from 2.1% to 3.0% of total LFOC in March 2009, and apparent turnover times of C3-derived LFOC ranged from 21 to 32 y for the sandy soils studied. Overall, our study indicates that stocks of LFOC and LFON in a sandy arable soil are temporarily too variable to obtain robust significant treatment effects of fertilizer type and rate at common agricultural practices within a season, despite the use of bulked six individual cores per plot, a common number of field replicates of four, and a length of treatments (28 y) in the order of the turnover time (21–32 y) of C3-derived LFOC.
机译:密度分级法的应用是一种成熟的技术,但是对不稳定土壤组分的短期动力学的研究很少。目的是(1)量化土壤C和N在轻组分(LFOC,LFON,ρ≤2.0g·cm –3 )和微生物量C(C中的长期和短期动态(sub)mic )在沙质Cambisol中受28年不同施肥的影响,并且(2)确定在一个生长季节中C 4 -C掺入这些不稳定组分中苋菜。处理方法为:秸秆还田加矿物肥料(MSI)施用和农家粪肥(FYM)的施用分别在高(MSI H ,FYM H ,140–150 kg N ha –1 y –1 )和低(MSI L ,FYM L ),50–60 kg N四个场重复的ha –1 y –1 )速率。对于2008年(3月,5月和9月)的所有三个采样日期,LFOC,LFON和C mic 的库存量按FYM H L的顺序减少 H ,MSI L 。但是,抽样日期之间的统计显着性差异显着,例如,LFOC按照上述顺序(3月的抽样日期)显着不同(p≤0.05),根据肥料类型(5月)或不重要(9月)而显着不同。 )。 LFOC在土壤有机碳储量中的比例很高(45%至55%),表明沙质Cambisol矿物表面上土壤有机物稳定的能力较低。在四种growing菜生长期中,a菜的一个生长季中,LFOC中C 4 -C的掺入量很小,占总量的2.1%至3.0% 2009年3月的LFOC,C 3 衍生的LFOC的表观转换时间在21到32 y范围内。总体而言,我们的研究表明,尽管每个耕地使用散装的六个独立核心,但沙质耕地中的LFOC和LFON的存量暂时变化太大,无法在一个季节内的常规农业实践中获得强大的肥料类型和施用量的显着处理效果,常见的野外重复数为4,并且处理时间(28 y)的顺序为C 3 衍生的LFOC的转换时间(21–32 y)。

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