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1.
Abstract. The Pan‐European Soil Erosion Risk Assessment (pesera ) model was evaluated using existing soil erosion data collected under various types of climate, vegetation, landscape and soil conditions. The data used represent a variety of typical Mediterranean land uses such as winter wheat, vines, olives and bare, stony land prevailing in hilly areas. Using this data, the model was calibrated for sediment transport by overland flow and results compared to measured soil erosion values from runoff plots and a watershed on a monthly basis. The performance of the model was assessed statistically, showing that it can be satisfactorily used for predicting soil erosion rates under the conditions included in the study. The overall model estimate including all the available experimental data was 0.69 t ha?1 yr?1 with a maximum error of 1.49 t ha?1 yr?1. After validation, the model was applied to a small watershed (60 ha) of great ecological importance for the sea turtle Caretta caretta. For this purpose, soil and vegetation maps were compiled from all the necessary data for applying the model. The model was run for three years using daily data from an existing nearby meteorological station. The predicted and measured soil erosion rates for a 7‐month period were 0.31 t and 0.18 t, respectively. Application of the model to each mapping unit showed the over‐riding importance of land use for sediment generation under the given climatic conditions. Bare land, occupying 5.5% of the watershed area, generated up to 69% of the total sediments estimated for the watershed. It is concluded that the pesera model can be used as a regional diagnostic tool under a range of soil, topographic and climatic conditions for identifying the best land use type and vegetation cover to protect hilly areas from soil erosion. The calculated overall root mean square error for the model is 0.06 t ha?1 yr?1, compared to a soil erosion rate of 0.04 t ha?1 yr?1, which can be tolerated for protecting the area for the sea turtle. 相似文献
2.
杨雨行 《北京林业大学学报》1995,(1)
依据航片判读、森林资源调查资料和水文数据,利用流域自身对比法,得出森林变化对河川径流泥沙的定量关系。文中还阐明本方法的技术关键——消除降雨量不同对水沙的影响.该方法具有适合我国国情、费小效宏、精度较高、简捷易行等优点,值得推广提倡。 相似文献
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INTRODUCTIONAtpresent,oxygenbleachinghasbecomeanlndustrializedtechnolOgy.Uptol989,thistechnologyhadbeenusedin58paPerndlls,and50%ofthemwereinEuroPe,20%inNorthemAmencaand20%inJapan.Inrecentyears,severaloxygnbleachiofequiPmenthadbeenintroducedintoChina.Inaword,oxygenbleachinglsasuccessfulandenviron-mentallyaccePtableprocessfOrPulpbleaching.However,littleworkhadbeendevotedtounderstandingthefundamentalaspectsofthissysten1,sotherewaslittledetailedinfOrmationonthel11echanismsofoxygenbleachi… 相似文献
4.
全子叶生物活性豆腐凝胶特性的研究 总被引:1,自引:0,他引:1
通过因子筛选实验,确定了接种量、微生物转谷氨酰胺酶(MTG)用量和水豆比是影响全子叶生物活性豆腐凝胶特性的关键因子。在此基础上,采用响应曲面法(Response SurfaceMethodology,RSM)分别建立了豆腐硬度和持水率的二次多项数学模型,验证了模型的有效性并探讨了上述3个因子的交互作用。从产品成本和凝胶特性综合考虑,选择出最佳配比,即乳酸菌接种量为105cfu/mL,MTG用量为347 U/L,水豆比为8.5,其硬度和持水率实测值分别为44.8g和89.2%,可生产出富含乳酸菌和几乎全部大豆营养的健康豆腐。 相似文献
5.
海湾泥碱渣和粉煤灰作为园林种植基质的氮素生理类群及生化作用研究 总被引:4,自引:1,他引:3
海湾泥、碱渣和粉煤灰是天津滨海地区大量存在的固体废弃物,通过前期室内配比筛选、盆栽试验、田间试验表明其混合基质可以用于园林绿化,并在防护林建设中获得成功.以滨海盐土、客土绿地为对照,对通过脱盐、培肥、种植毛白杨、刺槐、洋白蜡、金银木、紫花苜蓿等园林植物后基质的氨化细菌、好气性自身固氮菌、硝化细菌、反硝化细菌、纤维素分解菌等土壤氮素生理类群的数量进行了研究,同时对呼吸作用、氨化作用强度以及二者与土壤微生物数量、理化性质进行了相关性分析.结果表明,基质的氮素生理类群数量高于或与客土绿地相当,明显高于滨海盐土.呼吸作用高于客土绿地和滨海盐土,氨化作用强度与客土绿地相当,说明混合基质的氮素转化、有机物质的矿化能力以及基质整体的代谢水平好于客土绿地.土壤呼吸作用强度与土壤盐分呈极显著负相关,与细菌数量呈显著正相关.氨化作用强度与全氮、全磷、有机质含量、细菌和真菌数量呈极显著正相关,与放线菌呈显著正相关,与速效钾、盐分呈显著负相关. 相似文献
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8.
提出一种基于点云数据的NURBS曲面重建方法,针对数据点的分布不均匀性,进行非均匀B样条曲线控制点的反算,通过累积弦长法构造非均匀节点矢量,保证了曲面的插值精度和曲面重建的质量。 相似文献
9.
瓦埠湖沉积物氮的赋存特征以及环境因子对NH4+-N释放的影响 总被引:9,自引:1,他引:8
采用现场采样和室内测试的方法,研究了瓦埠湖沉积物各层的TN、NH4^+-N、NO3^--N的赋存特征。结果发现,TN上层比底层低,随着沉积深度的增加,硝化作用相对减弱,NO3^-N随着沉积深度的增加而减少,NH4^+-N的含量随着沉积深度的增加而增加。pH〈9时,pH对NH4^+-N释放的影响规律不是很明显,pH〉9时,NH4^+-N释放随着pH的增加而增加。随着温度的升高,NH4^+-N的释放量增大。好氧、厌氧条件下,NH4^+-N都有释放,且在好氧条件下NH4^+-N呈低释放状态,厌氧状态下NH4^+-N呈高释放状态。 相似文献
10.
Effects of structural and depositional crusts on soil erosion on the Loess Plateau of China 总被引:2,自引:0,他引:2
Conventional tillage practices used on the Loess Plateau lead to different soil surface micro-topography which results in forming two types of soil crusts. The objective of this study was to explore the formation position, properties and erosion characteristics of structural crusts and depositional crusts under the influences of the microtopography in the rainfall experiments. Two simulated rainstorms were applied in the experiments. The first rainfall event was used for soil crust formation, then the following simulated rainfall storms at 40 mm h?1, 60 mm h?1, and 80 mm h?1 rates were applied to the soil boxes set to a 17.6% (10°) slope under three tillage types (contour tillage, artificial digging, and straight slope conditions) to investigate the resulting runoff discharge rate and sediment yield on crusted soil surface. Results show that: (1) structural crusts formed on the mounds, and depositional crusts formed in the depressions after the first rainfall events; structural crusts exhibit a lower thickness, bulk density, higher porosity and shear strength than depositional crusts; (2) structural crusts increased the runoff yield less and decreased the sediment yield more than depositional crusts; and (3) the runoff yield was significantly greater, and the sediment yield was lower on the crusted soil surface than that on the uncrusted soil surface, regardless of the effect of the tillage treatments. 相似文献