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首页> 外文期刊>Nutrient Cycling in Agroecosystems >Influence of different land-cover types on the changes of selected soil properties in the mountain region of Rawalakot Azad Jammu and Kashmir
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Influence of different land-cover types on the changes of selected soil properties in the mountain region of Rawalakot Azad Jammu and Kashmir

机译:拉瓦拉科特·阿扎德·查mu和克什米尔山区不同土地覆被类型对某些土壤性质变化的影响

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The study focused on the impact of change in land-cover types on soil quality inferred by measuring the relative changes in chemical and physical properties of non-disturbed and disturbed soil system.Soil samples were collected from major land-cover types in the mountain region:natural forest,grassland and cultivated land (arable).The natural forest served as a control against which to assess changes in soil properties resulting from the removal of natural vegetation or cultivation of soil.Soil samples were collected from 0-15 and 15-30 cm depth six times during the year and examined for their nutrient status,i.e.soil organic matter (SOM);total N (TN);available P (AP);available K (AK);cation exchange capacity (CEC),pH and physical properties like particle size distribution,bulk density (BD),and porosity.Significant differences among land-cover types were found for SOM,TN,AP;AK,CEC and pH.Soil collected from the forest had the highest levels of all nutrients followed by grassland while soil from the arable site had very low nutrient status indicated an extractive effect of cultivation and agricultural practices on soil.With significantly lower clay contents (20%),texturally the soil of arable site was quite different from that of the natural forest and grassland.Similarly,a 13% more BD and 12% lower porosity showed structural deterioration of arable soil.The changes in clay contents,BD and porosity due to cultivation suggest adverse effects on environmental protection functions of soil.The correlation coefficient between OM to TN,AP,AK and CEC suggesting that within a narrow range of soil,OM may serves as a suitable indicator of soil quality.Natural vegetation appeared to be a main contributor of soil quality as it maintained the organic carbon stock and increased the nutrient status of soil and is therefore,important to sustain high-altitude ecosystems and reinstate the degraded lands in the mountain region.
机译:通过测量未扰动和扰动土壤系统的化学和物理性质的相对变化,研究着重于土地覆盖类型的变化对土壤质量的影响。从山区主要土地覆盖类型中收集土壤样品:天然林,草地和耕地(耕地)。以天然林为对照,评估因去除天然植被或土壤耕种而导致的土壤性质变化。从0-15和15-一年中六次30厘米深度,检查其养分状况,土壤有机质(SOM);总氮(TN);有效磷(AP);有效钾(AK);阳离子交换容量(CEC),pH和物理性质如粒度分布,堆积密度(BD)和孔隙率.SOM,TN,AP,AK,CEC和pH在土地覆盖类型之间存在显着差异。从森林收集的土壤中所有养分含量最高其次是草原耕地土壤的养分含量很低,说明耕作和农业实践对土壤具有萃取作用。粘土含量低得多(20%),从质地上讲,耕地土壤与天然森林和草原有很大不同。同样,BD增加13%,孔隙率降低12%表明耕作土壤的结构恶化。耕作引起的粘土含量,BD和孔隙率的变化表明对土壤的环境保护功能有不利影响.OM与TN,AP之间的相关系数,AK和CEC表明,在狭窄的土壤范围内,OM可以作为土壤质量的合适指标。自然植被似乎是土壤质量的主要贡献者,因为它可以保持有机碳库并增加土壤和土壤的养分状况。因此,对于维持高海拔的生态系统和恢复山区退化的土地至关重要。

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