长期草地管理下退化耕地力学与弹性特征的变化

Ayodele Ebenezer Ajayi, Oluwaseun Temitope Faloye, Jens Rostek, Veronika Schroeren, Abayomi Fasina, Rainer Horn
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引用次数: 0

摘要

为满足日益增长的粮食、饲料和纤维需求而持续集约化的农业生产加剧了土壤变形,从而加速了土壤退化。为恢复土壤功能,建议将部分退化耕地转为永久草地。然而,在了解退化土地的稳定性(对干扰的抵抗力和恢复力)有效恢复的时间表方面,仍然存在相当大的差距。此外,改良草地恢复过程的动态仍不完全清楚。研究了改良草地改造1年、2年、8年、13年、19年和25年后退化耕地3个不同深度(0-5、10-15和20-25 cm)土壤的物理、水力和力学性能,包括压缩系数(Cn)和预压应力。为了充分理解并最终确定自改进转换以来作为时间函数的恢复过程的动态,我们结合了来自预排至- 60 hPa基质电位的样品的2组不同测量(加载条件)的分析数据。加载条件为:(a)静约束压缩,施加4 h的正应力,分别为1、20、50、100、200和400 kPa,每个样品没有应力松弛,以及(b) 50 kPa的动态循环加载,加载和卸载30 秒(松弛)。我们纳入了关于循环加载条件下孔隙水压力动态的数据,以记录弹性可能的变化。结果表明,加载过程中的沉降和卸载过程中的弹性回弹与地表年龄和取样深度有关。在循环加载试验前,老桩有效应力值较高,加载后有效应力值随孔隙水压力的变化而变化。加载时有效应力值小于卸载时的负应力值。25年林龄草地在0 ~ 5 cm土层深度,由于土壤性质的变化,特别是土壤容重的变化,回弹率和压缩性系数较高,而在10 ~ 15和20 ~ 25 cm土层深度,其平均值更接近。当考虑回弹率时,最高的平均值出现在转换后的13年。另外,8年树龄的草木在静载作用下的预压应力值显著高于静载作用下的预压应力值,比静载作用下的预压应力值低19年。静载作用下,较高的预压应力多出现在较低深度处。最后,研究结果表明,转换为草地后,强度恢复和物理性质和功能恢复需要8 ~ 13年的时间。对于预压应力和顶部5 cm的土壤压缩性/回弹,甚至在20-25 cm的更深深度也观察到这种恢复
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Changes in mechanical and resilience characteristics of degraded arable land under long-term grassland management
The sustained intensification of agricultural production to meet increasing food, feed and fibre demands has aggravated soil deformation, thereby accelerating soil degradation. The conversion of some of these degraded arable lands to permanent grassland has been recommended to recover the soil functions. However, there is still a considerable gap in understanding the timeline for the effective recovery of degraded land in terms of its stability (resistance and resilience to disturbance). Moreover, the dynamics of the recovery process in ameliorative grasslands are still not fully understood. In this study, the physical, hydraulic, and mechanical properties including the coefficient of compressibility (Cn) and precompression stress were investigated in degraded arable land at three different depths (0–5, 10–15 and 20–25 cm) after 1-, 2-, 8-, 13-, 19-, and 25-years ameliorative grassland conversion. To fully understand and finalise the dynamics of the recovery process as a function of time since the amelioratory conversion, we combined the analysed data from 2 different sets of measurements (loading conditions) on samples predrained to − 60 hPa matric potential. The loading conditions were (a). static - confined compression with normal stresses applied for 4 h in steps of 1, 20, 50, 100, 200, and 400 kPa without stress relaxation on each sample, and (b). dynamic - cyclic loading at 50 kPa with 30 seconds of loading and unloading (relaxation). We included data concerning porewater pressure dynamics under the cyclic loading condition to document possible changes in elasticity. Our results showed that settlement during loading and the elastic rebound during unloading were related to the sward age and the sampled depth. Before the cyclic loading experiment, higher values of effective stress were recorded in the older swards, but the values changed after loading in response to the change in the porewater pressure. The effective stress values were less negative during loading than when unloading. At soil depth of 0–5 cm in the 25 years old sward, the rebound rate (values) and the coefficient of compressibility were higher due to changes in soil properties, particularly the soil bulk density, while at the 10–15 and 20–25 cm depths, the mean values were much closer. When the rebound rate was considered, the highest mean value occurred at 13 years after conversion. In addition, significantly higher values of pre-compression stress were observed in the 8-year-old sward under static loading, which decreased by 19 years. Higher values of pre-compression stress were mostly recorded at the lower depths under static loading. Finally, the results showed that a period between 8 and 13 years is needed to document the starting of strength regain and the recovery of the physical properties and functions, after conversion to grassland. This recovery was observed even up to deeper depths of 20–25 cm for precompression stress and for the soil compressibility/rebound in the top 5 cm
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