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首页> 外文期刊>Communications in Soil Science and Plant Analysis >Variations in Soil Physical Properties in a Cleared Forestland Continuously Cultivated for Seven Years in Eastern Nsukka, Nigeria.
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Variations in Soil Physical Properties in a Cleared Forestland Continuously Cultivated for Seven Years in Eastern Nsukka, Nigeria.

机译:尼日利亚东部Nsukka连续耕种了7年的砍伐林地的土壤物理特性变化。

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In this study, soil physical properties were evaluated in the top 40 cm of cleared forestland that had been subjected to continuous cultivation for 7 years to ascertain selected crop or crop combinations that influenced the soil physical properties the most. There was no significant effect of crop treatment on particle-size distributions over 6 years of cultivation. In year 7, clay values were significantly (p = 0.05) greater in plots grown with solely cassava (SC) and solely maize (SM) than in the plots grown with solely pigeon pea (SP). The soil depth effects over the 7 years were significant on the clay content. The mean values of bulk density, pore-size distribution, and hydraulic conductivity obtained from each plot fluctuated over the years. The bulk density values in 1998 ranged from 1.29 to 1.43 g cm3, but from 1999 to 2004, the range was from 1.12 to 1.40 g cm3. Thus, bulk density generally decreased when compared with their respective values in 1998. The greatest decrease of 22% was in 2000. More than 70% of the macroporosity values were significantly less than their respective values in 1998. The greatest decease of 72% was obtained from SM plots in 2001. All the microporosity were significantly more than the 1998 values. All the increases were >100% of the original values. These increases were reflected in the variations of total and saturated hydraulic conductivity (Ks) values. However, in 2004, Ks values decreased in the plots grown to C + P, SP, and SM. Generally, the C + M + P mixture appeared to be the most consistent in improving micro- and total porosities and Ks among the crop treatments.
机译:在这项研究中,对已经进行了连续耕种7年的40厘米开阔林地的土壤物理性质进行了评估,以确定对土壤物理性质影响最大的所选作物或作物组合。种植6年后,作物处理对粒径分布没有明显影响。在第7年,仅使用木薯(SC)和仅玉米(SM)种植的地块的黏土值显着(p = 0.05)高于仅使用木豆(SP)种植的地块。 7年来土壤深度的影响对粘土含量有显着影响。多年以来,从每个图获得的堆积密度,孔径分布和水力传导率的平均值都在波动。 1998年的堆积密度值在1.29至1.43 g cm3之间,而从1999年至2004年,则在1.12至1.40 g cm3之间。因此,与1998年的各自值相比,总体密度通常下降。最大的下降是在2000年,为22%。1998年,大孔隙率的值大大超过其各自值的70%。最大的下降是72%。从2001年的SM图获得。所有的微孔率都明显高于1998年的值。所有增加均大于原始值的100%。这些增加反映在总和饱和水力传导率(Ks)值的变化中。但是,在2004年,在成长为C + P,SP和SM的图中,Ks值下降了。通常,在作物处理中,C + M + P混合物似乎在改善微观和总孔隙率和Ks方面最一致。

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