东非茶区氮肥用量和采采间隔对土壤有机碳、pH和茶叶产量的影响及其关系

R. O. Ombori, P. Owuor, D. Kamau, B. O. Kwach, Wilson Dufitumukiza, S. Msomba
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引用次数: 0

摘要

东非茶叶生长在雨量充沛的地区,那里的营养物质因淋滤而枯竭,地表径流可能很高,此外还会随作物一起流失。因此,通过施肥补充养分是必要的。但施肥不当会导致养分失衡,改变土壤pH值和有机碳含量。采摘间隔的变化导致茶叶产量的差异。尽管东非茶叶种植区的环境因素各不相同,但推荐的肥料类型和用量以及收获间隔在很大程度上是一致的。肥料使用和收获政策对区域内土壤化学参数有不同程度的影响。评价了NPKS 25:5:5施肥量和采采间隔对东非地区土壤有机碳、pH的影响以及土壤有机碳、pH与茶叶产量的关系。TRFK 6/8无性系在Timbilil、Changoi、Arroket(肯尼亚)、Maruku、Katoke(坦桑尼亚)、Kitabi和Mulindi(卢旺达)进行了试验。土壤有机碳含量在4.16% ~ 17.61%之间,较为充足。施氮量的增加增加了土壤有机碳(p < 0.05),降低了土壤pH (p < 0.05), pH值在3.22 ~ 4.84之间。从长远来看,高施氮率导致的土壤酸度增加会降低茶叶的产量。在茶叶生产中,必须定期监测土壤pH值,以便在pH值低于3.5时启动缓解活动。采期对土壤有机碳和pH值均无显著影响。土壤有机碳和pH值在可接受范围内,但在不同地点差异显著(p≤0.05)。土壤有机碳直接相关(r >0.878);除Mulindi和Maruku外,所有地点的土壤有机碳含量p均小于或等于0.05,而ph与产量呈负相关(r小于或等于-0.878,大多数地点的土壤有机碳含量p小于或等于0.05)。有机碳含量与产量之间的相关性表明,茶叶生产管理需要将有机碳含量维持在最佳水平,以实现茶叶的持续产量。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Nitrogenous Fertilizer Rates and Plucking Intervals Effects on Soil Organic Carbon, pH and Tea Yields and Their Relationships in Eastern Africa Tea Growing Regions
Eastern Africa tea grows in high rainfall areas where nutrients depletion through leaching, and surface run-off can be high, in addition to removal with crop. Nutrients replenishment through fertilizer applications is therefore necessary. But inappropriate fertilizer use can cause nutrients imbalance, change soil pH, and organic carbon contents. Variations in plucking intervals result in differences in tea productivity. Although environmental factors vary within Eastern Africa tea growing regions, recommended fertilizer type and rates and harvesting intervals are largely uniform. Fertilizer use and harvesting policy may influence soil chemical parameters within the region to varying degrees. Effects of NPKS 25:5:5:5 fertilizer rates and plucking intervals on soil organic carbon, pH and the relationship between soil organic carbon, pH and tea yields in Eastern Africa were evaluated. Trials were conducted on clone TRFK 6/8 at Timbilil, Changoi, Arroket (Kenya), Maruku, Katoke (Tanzania), Kitabi and Mulindi (Rwanda). Soil organic carbon contents ranged from 4.16 to 17.61% and were sufficient. Increasing nitrogen rates increased (p less than or eqaul to 0.05) soil organic carbon but lowered (p less than or eqaul to 0.05) soil pH. The pH values ranged between 3.22 and 4.84. The increase in soil acidity due to high rates of nitrogen rates reduce tea productivity in the long run. Periodic monitoring of soil pH is necessary in tea production to invoke mitigation activities when decline below 3.5. Plucking intervals had no influence on SOC and pH at all sites. Soil organic carbon and pH varied significantly (p less than or eqaul to 0.05) from location to location, though the values were within acceptable range. Soil organic carbon directly correlated (r.>0.878; p less than or eqaul to 0.05 for all sites except Mulindi and Maruku) with yields and inversely (r less than or eqaul to -0.878, p less than or eqaul to 0.05 for most sites) with pH. The correlation between SOC and yields suggest that tea production management need to maintain SOC at optimal levels realization of sustained tea yields.
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