首页> 外文期刊>Geoderma: An International Journal of Soil Science >Response of shallow karst fissure soil quality to secondary succession in a degraded karst area of southwestern China
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Response of shallow karst fissure soil quality to secondary succession in a degraded karst area of southwestern China

机译:中国西南部退化喀斯特地区浅岩溶裂缝土壤质量对浅岩溶裂缝土壤质量的影响

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摘要

Vegetation restoration is one of the effective means to control soil erosion and an essential method of eco-environmental restoration in fragile karst rocky desertification areas. The shallow karst fissure (SKF) filled with soil has become one of the most important root habitats in this area. It is essential to scientifically evaluate the soil quality of SKF and to provide a basis for matching species with sites. Here, we explore and gain insight into the characteristics of the response of the physicochemical properties of SKF soil to different stages of vegetation succession. Additionally, we develop a synthetical assessment system to determine soil quality. The key results were as follows. Significant differences were found in the soil properties between the surface and the SKF. Compared with the surface, the SKF soil structural property was poor, but the water conditions were better. The soil nutrient content of the SKF was significantly (p 0.05) lower than that of the surface, but the differences in soil nutrients inside the SKF were not significant. In addition, the soil quality indicator (SQI) values of the SKF soil were significantly (p 0.05) lower than those of the surface and decreased gradually with soil depth. Moreover, secondary succession significantly (p 0.05) improved the soil properties and, thus, the soil quality. With recovery of vegetation, the soil properties of the surface and the SKF were significantly improved. The difference in the soil properties and the SQI values between the surface and underground gradually narrowed with succession. Furthermore, the thickness of the SKF soil was more than twice that of the surface soil. Overall, the soil properties and the soil quality of the SKF were relatively poor, but they were greatly improved with vegetation restoration. The SKF habitat can be the preferred habitat for vegetation restoration and is more favourable for plants with deep roots and a higher root penetration ability. The results of this study can supply references for future studies on karst rocky desertification control and vegetation restoration in the karst area of southwestern China, northern and central Vietnam, the islands of Java, Indonesia and Kampot Province, southwestern Cambodia and other karst regions with the same ecological background.
机译:植被恢复是控制土壤侵蚀的有效手段之一,以及在脆弱的喀斯特岩石荒漠化区域中生态环境恢复的必要方法。充满土壤的浅岩溶裂缝(SKF)已成为该地区最重要的根栖息地之一。必须科学评估SKF的土壤质量,并为匹配物种提供匹配物种的基础。在这里,我们探索并深入了解SKF土壤物理化学性质对植被连续不同阶段的响应的特征。此外,我们还开发了一种综合评估系统来确定土壤质量。关键结果如下。在表面和SKF之间的土壤性质中发现了显着差异。与表面相比,SKF土壤结构性差,但水条件较好。 SKF的土壤养分含量显着(P <0.05)低于表面的含量,但SKF内的土壤营养素的差异不显着。此外,SKF土壤的土壤质量指标(SQI)值明显(P <0.05)低于表面的水平,并用土壤深度逐渐降低。此外,二次继承显着(P <0.05)改善了土壤性质,从而改善了土壤质量。随着植被的恢复,表面和SKF的土壤性质显着提高。土壤性质的差异和地面与地下之间的SQI值逐渐缩小。此外,SKF土壤的厚度大于表面土壤的两倍。总体而言,土壤性质和SKF的土壤质量相对较差,但它们与植被恢复大大提高。 SKF栖息地可以是植被恢复的首选栖息地,对具有深层根深蒂固的植物和较高的根渗透能力更有利。本研究的结果可以为中国西南,越南喀斯特地区,越南喀斯特地区,印度尼西亚岛,柬埔寨西南部等喀斯特省和其他喀斯特地区以及其他喀斯特地区的喀斯特地区的喀斯特岩石荒漠化控制和植被恢复的研究结果提供了对喀斯特岩石荒漠化控制和植被恢复的参考相同的生态背景。

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