首页> 外文期刊>Archives of Agronomy and Soil Science >Stratification of mineral-N, P, K and organic C in the vertisols as affected by tillage systems
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Stratification of mineral-N, P, K and organic C in the vertisols as affected by tillage systems

机译:耕作系统对凡尔松中氮,磷,钾和有机碳的矿化作用

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Field experiments were conducted from 1996 through 2001 with a fixed layout. Cotton was sown within 2-5 cm of the previous years (60 cm row spacing). At the end of six years, soil was sampled from different depths (0-7.5, 7.5-15 and 15-30 cm) and positions (within planted row and between rows) of the three tillage systems namely, conventional tillage (CT), reduced tillage-1 (RT_1) and reduced tillage-2 (RT_2). The soil samples were analyzed for mineral-N, available P. exchangeable K and soil organic C (SOC). Continuous application of fertilizers within a planted row resulted in horizontal and vertical stratification of nutrients. Tillage effect was not significant but depth effect was highly significant for exchangeable NH_4~+, available P. exchangeable K and SOC. The nutrient content declined with increasing depth. Nitrate content was almost uniform through out the soil depth (0-30 cm) indicating its mobile nature. In general, fertilizer nutrient content was more within a planted row (WR) thanthe between row (BR) sampling position. The differences were significant for NO_3~-, NH_4~+ and exchangeable K~+. Tillage X position, tillage X depth X position interactions were highly significant for nitrate, ammonium, available P and exchangeable K. Within row surface layer (0-7.5 cm) of the RT plots, generally, had greater amount of exchangeable NH_4~+, available P and exchangeable K compared to the CT plots. SOC declined with depth, however, it was not affected by tillage and sampling position. Although no change in soil lest rating was evident after six years, positional application of fertilizers may affect the nutrient status and may warrant a change in the fertilizer recommendation to cotton.
机译:从1996年到2001年以固定布局进行了现场实验。在前几年的2-5厘米(行距60厘米)内播种了棉花。在六年结束时,从三种耕作系统的不同深度(0-7.5、7.5-15和15-30 cm)和位置(种植行内和行间)对土壤进行了采样,即常规耕作(CT),减少耕种1(RT_1)和减少耕种2(RT_2)。分析土壤样品中的矿质氮,有效的可交换磷和土壤有机碳(SOC)。在种植行中连续施用肥料会导致养分的水平和垂直分层。对于可交换的NH_4〜+,可利用的P.可交换的K和SOC,耕作效果不显着,但深度效果高度显着。养分含量随深度增加而下降。在整个土壤深度(0-30厘米)内,硝酸盐含量几乎是均匀的,表明其具有流动性。通常,种植行(WR)内的肥料养分含量高于行间(BR)采样位置的肥料养分含量。对于NO_3〜-,NH_4〜+和可交换的K〜+,差异显着。对于硝酸盐,铵盐,有效磷和可交换钾,耕作X位置,耕作X深度X位置之间的相互作用非常显着。在RT图的行表层(0-7.5 cm)内,总的可交换NH_4〜+量较大,与CT图相比,可用P和可交换K。 SOC随深度下降,但不受耕种和取样位置的影响。尽管六年后土壤肥力等级没有明显变化,但肥料的定位施用可能会影响养分状况,并可能需要改变对棉花的肥料推荐量。

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