首页> 外文期刊>Indian Journal of Forestry >Changes in the physico-chemical properties of soil under shifting cultivation with special reference to karbi anglong district of Assam
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Changes in the physico-chemical properties of soil under shifting cultivation with special reference to karbi anglong district of Assam

机译:特别是阿萨姆邦karbi anglong区轮作栽培下土壤理化性质的变化

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The effect of shifting cultivation on changes in the physico-chemical properties of soils was studied in the jhum and nearby natural forest areas. Various soil properties investigated were bulk density, texture, pH. hydraulic conductivity, organic carbon, total nitrogen, available phosphorus and exchangeable potassium, calcium and magnesium. Soil properties were compared at five different soil depths: 0-5 cm, 5-25 cm, 25-50 cm, 50-100 cm and 100~+ cm. Lowest and highest soil bulk densities were recorded in land after burning and 1st year fallow, respectively. Natural forest had a moderate soil bulk density. Results indicate that C and N in the soil may be among the most limiting factors for plant growth after a forest is cut and burned. Highest percentage of organic carbon (1.92 percent) and total nitrogen (0.28 percent) were found in pre-burning stages of vegetation and it significantly decrease in early fallow periods due to rejuvenation of vegetation. With the progress in the age of fallow, the percentage of organic carbon and total nitrogen increased significantly due to heavy accumulation of litterfall. A large amount of available phosphorus is released just after burning the forest. The lowest value of available phosphorus found in 1st and5th year fallows indicate that available phosphorus may limit crop production if the fallow periods are too short. Maximum amount of available phosphorus noticed in natural forest is due to heavy accumulation of litterfall. Exchangeable calcium, potassium and magnesium appeared to reach adequate levels in the soil after burning the forest and sharply declined in cropping period and it continuously decreased in early successional fallow. Natural forest exhibited adequate levels of exchangeable calcium,potassium and magnesium, while increase in 15th and 20th years fallow may be due to development of regeneration of tree vegetation. The overall results of this study indicate that the present shifting cultivation cycle of about 5 years is not sufficientto prevent serious soil degradation in the area. A minimum of 10 to 15 years will be required to maintain soil fertility at a reasonable level.
机译:在乔木及其附近的天然林地区,研究了轮作对土壤理化性质变化的影响。研究的各种土壤特性包括堆积密度,质地,pH。水力传导率,有机碳,总氮,有效磷以及可交换的钾,钙和镁。在五个不同的土壤深度下对土壤特性进行了比较:0-5 cm,5-25 cm,25-50 cm,50-100 cm和100〜+ cm。燃烧后和第一年休耕后,最低和最高土壤容重分别记录在土地上。天然林的土壤容重中等。结果表明,森林砍伐和燃烧后,土壤中的碳和氮可能是植物生长的最大限制因素。在植被的燃烧前阶段发现了最高的有机碳百分比(1.92%)和总氮(0.28%),并且由于植被的复兴,其在休耕初期显着减少。随着休耕年龄的增长,由于凋落物的大量积累,有机碳和总氮的百分比显着增加。燃烧森林后,大量的有效磷释放出来。在第一年和第五年休耕期发现的可用磷最低值表明,如果休耕期太短,则可用磷可能会限制作物的生产。天然林中发现的最大有效磷含量是由于凋落物的大量积累。烧毁森林后,土壤中的交换性钙,钾和镁似乎已达到适当水平,并在种植期急剧下降,并在连续演替休耕期持续下降。天然林中钙,钾和镁的交换水平足够,而第15年和第20年休耕期的增加可能是由于树木植被的再生所致。这项研究的总体结果表明,目前大约5年的轮换种植周期不足以防止该地区严重的土壤退化。至少需要10至15年才能将土壤肥力维持在合理水平。

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