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Organic resources quality and soil fauna: their role on the microbial biomass, decomposition and nutrient release patterns in kenyan soils

机译:有机资源质量和土壤动物区系:它们对肯尼亚土壤微生物生物量,分解和养分释放模式的作用

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Five organic resources commonly used for soil fertility maintenance in large parts of Kenya were selected for litter decay and nutrient mineralization studies that were conducted in three farms (Machakos, Kabete and Njabini) located at an elevational transect ranging from 1500 to 2800 m above sea level. These organic residues included: bean trash, maize stover, tree prunnings (Grevillea robusta), Senna spectabilis foliage, cow and poultry manures. Organic residues were either mulched or incorporated in the soil. Satellite experiments were also carried out in each of the three sites with one additional site at Maseno based in western Kenya. These experiments aimed at assessing the role of soil biota in the decomposition and nutrient release. Soil fauna were excluded from control plots using 1-mm mesh litterbags. The organic residues were different in chemical composition i.e. nitrogen (N), phosphorus (P), potassium (K), carbon (C), lignin (L) and polyphenol (PP) contents, which in turn influenced their rate of decomposition and nutrient release patterns. Bean trash decomposed and released N and P faster than either the maize stover or Grevillea prunings. The slowest rate of decomposition observed for Grevillea prunings could be attributed to the high lignin content (24%). The N release was influenced by (L+PP):N ratio. Bean trash having a ratio of 10 released N faster than either maize stover or Grevillea prunings whose respective ratios of 20 and 13. P release was influenced by both C:P and N:P ratios. Maize stover with C:P and N:P ratios that were higher than the critical levels of 123 and 10 respectively, mineralized and released P more slowly than either bean trash or Grevillea prunings. Incorporated materials decomposed and released nutrients faster than surface applied materials. For surface applied organic materials, the delay in litter decay ranged from 4.1 to 4.4 days for every 100 m increase in altitude, while for incorporated materials the delay in litter decay ranged from 1 to 3 days per 100 m increase in elevation. This implies that farmers at higher elevations would benefit more by incorporating residues before planting, while at low elevations post emergence surface application would lead to improved nutrient availability. Njabini and Kabete recorded significantly higher microbial biomass (C, N and P) than Machakos. This could be linked to the higher organic C, higher total N, higher moisture content but lower temperatures reported for Njabini and Kabete than Machakos. Soil fauna enhanced decomposition of organic residues, although their role in influencing nutrient availability to crops from the organic residues may depend on the nature of the material. Fauna had no significant influence on nutrient release patterns of Senna possibly due to secondary compounds present in Senna, which were lower than the critical levels of 15 for lignin and 4 for polyphenol respectively.
机译:选择了肯尼亚大部分地区通常用于维持土壤肥力的五种有机资源,用于凋落物腐烂和养分矿化研究,这些研究在海拔1500至2800 m的高海拔断面的三个农场(Machakos,Kabete和Njabini)进行。这些有机残留物包括:豆类垃圾,玉米秸秆,树木修剪(Grevillearobusta),番泻叶,牛和家禽粪便。将有机残留物覆盖或掺入土壤中。在这三个地点中的每个地点都进行了卫星实验,并在肯尼亚西部的Maseno增设了一个地点。这些实验旨在评估土壤生物在分解和养分释放中的作用。使用1毫米网孔垃圾袋将土壤动物从控制区中排除。有机残留物的化学成分不同,即氮(N),磷(P),钾(K),碳(C),木质素(L)和多酚(PP)含量,进而影响了它们的分解速率和养分释放模式。豆类垃圾的分解和释放N和P的速度比玉米秸秆或Grevillea修剪的速度要快。 Grevillea修剪观察到的最慢的分解速率可能归因于高木质素含量(24%)。氮的释放受(L + PP):N比的影响。比例为20的玉米秸秆或Grevillea修剪的比例为10的豆类垃圾释放N的速度更快,P的释放受C:P和N:P比率的影响。 C:P和N:P比率分别高于123和10的临界水平的玉米秸秆,其矿化和释放P的速度比豆垃圾或Grevillea修剪的慢。掺入的材料分解和释放的养分比表面施用的材料快。对于表面施用的有机材料,每增加100 m海拔,凋落物腐烂的延迟范围为4.1至4.4天,而对于掺入材料,每增加100 m高度,凋落物腐烂的延迟范围为1至3天。这意味着较高海拔的农民通过在种植前掺入残留物将受益更多,而较低海拔的农民出苗后施用表面肥料将改善养分利用率。 Njabini和Kabete记录的微生物生物量(C,N和P)明显高于Machakos。与Machakos相比,Njabini和Kabete的有机碳含量更高,总氮含量更高,水分含量更高,但温度却更低。土壤动物区系增强了有机残留物的分解,尽管它们在影响有机残留物对农作物的养分利用率方面的作用可能取决于材料的性质。动物区系对塞纳的养分释放模式没有显着影响,可能是由于塞纳中存在的次要化合物引起的,该次要化合物分别低于木质素的临界水平(15)和多酚的临界水平(4)。

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