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首页> 外文期刊>Agroforestry Systems >Carbon, nitrogen, organic phosphorus, microbial biomass and N mineralization in soils under cacao agroforestry systems in Bahia, Brazil
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Carbon, nitrogen, organic phosphorus, microbial biomass and N mineralization in soils under cacao agroforestry systems in Bahia, Brazil

机译:巴西巴伊亚州可可农林业系统下土壤中的碳,氮,有机磷,微生物生物量和氮矿化

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Large amounts of plant litter deposited in cacao agroforestry systems play a key role in nutrient cycling. Organic matter, nitrogen and phosphorus cycling and microbial biomass were investigated in cacao agroforestry systems on Latosols and Cambisols in Bahia, Brazil. The objective of this study was to characterize the microbial C and N, mineralizable N and organic P in two soil orders under three types of cacao agroforestry systems and an adjacent natural forest in Bahia, Brazil and also to evaluate the relationship between P fractions, microbial biomass and mineralized N with other soil attributes. Overall, the average stocks of organic C, total N and total organic P across all systems for 0-50 cm soil depth were 89,072, 8,838 and 790 kg ha-1, respectively. At this soil depth the average stock of labile organic P was 55.5 kg ha-1. For 0-10 cm soil depth, there were large amounts of microbial biomass C (mean of 286 kg ha-1), microbial biomass N (mean of 168 kg ha-1) and mineralizable N (mean of 79 kg ha-1). Organic P (total and labile) was negatively related to organic C, reflecting that the dynamics of organic P in these cacao agroforestry systems are not directly associated with organic C dynamics in soils, in contrast to the dynamics of N. Furthermore, the amounts of soil microbial biomass, mineralizable N, and organic P could be relevant for cacao nutrition, considering the low amount of N and P exported in cacao seeds.
机译:可可农林业系统中沉积的大量植物凋落物在养分循环中起关键作用。在巴西巴伊亚州的Latosols和Cambisols上的可可农林业系统中调查了有机物,氮和磷的循环以及微生物的生物量。这项研究的目的是在巴西巴伊亚州的三种可可农林业系统和相邻的天然林中,表征两个土壤阶中的微生物碳和氮,可矿化氮和有机磷,并评估磷组分与微生物之间的关系。生物质和矿化氮以及其他土壤属性。总体而言,在0至50 cm的土壤深度下,所有系统的平均有机碳,总氮和总磷分别为89,072、8,838和790 kg ha -1 。在该土壤深度下,不稳定有机磷的平均蓄积量为55.5 kg ha -1 。在0-10 cm的土壤深度中,存在大量的微生物生物量C(平均286 kg ha -1 )和大量的微生物生物量N(平均168 kg ha -1 ) >)和可矿化的氮(平均79千克ha -1 )。有机磷(总的和不稳定的)与有机碳呈负相关,反映出这些可可农林业系统中有机磷的动态与土壤中的有机碳动态不直接相关,与氮的动态相反。考虑到可可种子中氮和磷的出口量少,土壤微生物生物量,可矿化氮和有机磷可能与可可营养有关。

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