Teresa Palominos-Rizzo , Mario Villatoro-Sánchez , Darwin Paguada-Pérez , Alfredo Alvarado-Hernández , Víctor Cortés-Granados , Silvia Marín-Araya
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Nine runoff plots were installed in Llano Brenes, Costa Rica, in the upper basin of the Jesús María River in a study area with slopes between 50 and 71 ± 7.92 %. We conclude that this study could make an important contribution to research on the use of SWCM on tropical soils with slopes greater than 50 %. Due to the non-compliance of assumptions, a logarithmic transformation of the data was used, and they were evaluated using the Kruskal-Wallis one-way nonparametric test. Spearman correlation and linear regressions were used to assess the effect of the precipitation and intensity in the soil loss and runoff in each treatment. The amount of organic matter exposed by soil removal was not statistically different between HD and SCT, but both were different to the control (R<sup>2</sup> = 0.81, <em>P <</em> 0.05). Spearman correlation analysis showed the rainfall depth contributed more to runoff depth (HD <em>R</em> = 0.62; SCT <em>R</em> = 0.62; Control <em>R</em> = 0.60; <em>P <</em> 0.001) and soil loss (HD <em>R</em> = 0.50; STC <em>R</em> = 0.53; Control <em>R</em> = 0.50; <em>P <</em> 0.001) than other variables. Regression analysis showed that runoff and soil loss were significant (<em>P <</em> 0.05) and positively correlated with rainfall depth for each treatment. In this study, HD was shown to be efficient in erosion control on steeper slopes. HD helped reduce soil loss compared to the control, by 88 % in 2018 and 83 % in 2019. HD also reduced runoff generation by 55 % in 2018 and 60 % in 2019 compared to the control. While SCT was not statistically different in the generation of surface runoff and soil loss compared to the control.</p></div>","PeriodicalId":74839,"journal":{"name":"Soil security","volume":"14 ","pages":"Article 100128"},"PeriodicalIF":0.0000,"publicationDate":"2024-01-15","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"https://www.sciencedirect.com/science/article/pii/S2667006224000029/pdfft?md5=94f899b42d47ba1c566768b0ec6c5585&pid=1-s2.0-S2667006224000029-main.pdf","citationCount":"0","resultStr":"{\"title\":\"Effect of Staggered Contour Trenches and Hillside Ditches on surface runoff and soil loss on steep slopes in shaded coffee (Coffea arabica), Costa Rica\",\"authors\":\"Teresa Palominos-Rizzo , Mario Villatoro-Sánchez , Darwin Paguada-Pérez , Alfredo Alvarado-Hernández , Víctor Cortés-Granados , Silvia Marín-Araya\",\"doi\":\"10.1016/j.soisec.2024.100128\",\"DOIUrl\":null,\"url\":null,\"abstract\":\"<div><p>Soil erosion is one of the main causes of soil degradation and an important environmental problem, often accelerated by human activities. Different types of soil and water conservation measures (SWCM) have been implemented in worldwide to control soil loss, such as Staggered Contour Trenches (SCT) and Hillside ditches (HD) which are recommended in topographies up to 40 % slope. This study measured the effects of STC and HD, on surface runoff, soil loss, exposed of organic matter and soil moisture content, in a shaded coffee crop with steep slopes in an Entisol soil. Nine runoff plots were installed in Llano Brenes, Costa Rica, in the upper basin of the Jesús María River in a study area with slopes between 50 and 71 ± 7.92 %. We conclude that this study could make an important contribution to research on the use of SWCM on tropical soils with slopes greater than 50 %. Due to the non-compliance of assumptions, a logarithmic transformation of the data was used, and they were evaluated using the Kruskal-Wallis one-way nonparametric test. Spearman correlation and linear regressions were used to assess the effect of the precipitation and intensity in the soil loss and runoff in each treatment. The amount of organic matter exposed by soil removal was not statistically different between HD and SCT, but both were different to the control (R<sup>2</sup> = 0.81, <em>P <</em> 0.05). Spearman correlation analysis showed the rainfall depth contributed more to runoff depth (HD <em>R</em> = 0.62; SCT <em>R</em> = 0.62; Control <em>R</em> = 0.60; <em>P <</em> 0.001) and soil loss (HD <em>R</em> = 0.50; STC <em>R</em> = 0.53; Control <em>R</em> = 0.50; <em>P <</em> 0.001) than other variables. Regression analysis showed that runoff and soil loss were significant (<em>P <</em> 0.05) and positively correlated with rainfall depth for each treatment. In this study, HD was shown to be efficient in erosion control on steeper slopes. HD helped reduce soil loss compared to the control, by 88 % in 2018 and 83 % in 2019. HD also reduced runoff generation by 55 % in 2018 and 60 % in 2019 compared to the control. 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引用次数: 0
摘要
水土流失是土壤退化的主要原因之一,也是一个重要的环境问题,人类活动往往会加速这一问题的解决。为控制土壤流失,全球已实施了不同类型的水土保持措施(SWCM),如交错等高线壕沟(SCT)和山坡沟渠(HD),建议在坡度不超过 40% 的地形中使用。本研究测量了在 Entisol 土壤中的陡坡上种植遮荫咖啡作物时,STC 和 HD 对地表径流、土壤流失、有机质暴露和土壤水分含量的影响。在哥斯达黎加赫苏斯-玛丽亚河上游流域的拉诺-布雷内斯(Llano Brenes)设置了九个径流地块,研究区域的坡度在 50 到 71 ± 7.92 % 之间。我们的结论是,这项研究可以为在坡度大于 50% 的热带土壤上使用 SWCM 的研究做出重要贡献。由于不符合假设,我们对数据进行了对数变换,并使用 Kruskal-Wallis 单向非参数检验对数据进行了评估。斯皮尔曼相关和线性回归用于评估降水量和强度对各处理中土壤流失和径流的影响。在统计上,HD 和 SCT 因土壤清除而暴露的有机物数量没有差异,但两者与对照组相比都有差异(R2 = 0.81,P <0.05)。斯皮尔曼相关分析表明,与其他变量相比,降雨深度对径流深度(HD R = 0.62;SCT R = 0.62;对照 R = 0.60;P <;0.001)和土壤流失(HD R = 0.50;STC R = 0.53;对照 R = 0.50;P <;0.001)的影响更大。回归分析表明,在每种处理中,径流和土壤流失与降雨深度呈显著正相关(P <0.05)。这项研究表明,在较陡的斜坡上,HD 能有效控制水土流失。与对照组相比,HD 有助于减少土壤流失,2018 年减少了 88%,2019 年减少了 83%。与对照组相比,HD 还能减少径流的产生,2018 年减少 55%,2019 年减少 60%。而 SCT 与对照组相比,在产生地表径流和土壤流失方面没有统计学差异。
Effect of Staggered Contour Trenches and Hillside Ditches on surface runoff and soil loss on steep slopes in shaded coffee (Coffea arabica), Costa Rica
Soil erosion is one of the main causes of soil degradation and an important environmental problem, often accelerated by human activities. Different types of soil and water conservation measures (SWCM) have been implemented in worldwide to control soil loss, such as Staggered Contour Trenches (SCT) and Hillside ditches (HD) which are recommended in topographies up to 40 % slope. This study measured the effects of STC and HD, on surface runoff, soil loss, exposed of organic matter and soil moisture content, in a shaded coffee crop with steep slopes in an Entisol soil. Nine runoff plots were installed in Llano Brenes, Costa Rica, in the upper basin of the Jesús María River in a study area with slopes between 50 and 71 ± 7.92 %. We conclude that this study could make an important contribution to research on the use of SWCM on tropical soils with slopes greater than 50 %. Due to the non-compliance of assumptions, a logarithmic transformation of the data was used, and they were evaluated using the Kruskal-Wallis one-way nonparametric test. Spearman correlation and linear regressions were used to assess the effect of the precipitation and intensity in the soil loss and runoff in each treatment. The amount of organic matter exposed by soil removal was not statistically different between HD and SCT, but both were different to the control (R2 = 0.81, P < 0.05). Spearman correlation analysis showed the rainfall depth contributed more to runoff depth (HD R = 0.62; SCT R = 0.62; Control R = 0.60; P < 0.001) and soil loss (HD R = 0.50; STC R = 0.53; Control R = 0.50; P < 0.001) than other variables. Regression analysis showed that runoff and soil loss were significant (P < 0.05) and positively correlated with rainfall depth for each treatment. In this study, HD was shown to be efficient in erosion control on steeper slopes. HD helped reduce soil loss compared to the control, by 88 % in 2018 and 83 % in 2019. HD also reduced runoff generation by 55 % in 2018 and 60 % in 2019 compared to the control. While SCT was not statistically different in the generation of surface runoff and soil loss compared to the control.