基于迁移学习的棉花叶部病虫害图像识别

针对传统图像识别方法准确率低、手工提取特征等问题,该研究以棉花叶部病虫害图像为研究对象,利用迁移学习算法并辅以数据增强技术,实现棉花叶部病虫害图像准确分类。首先改进AlexNet模型,利用PlantVillage大数据集训练取得预训练模型,在预训练模型上使用棉花病虫害数据微调参数,得到平均测试准确率为93.50%;然后使用数据增强技术扩充原始数据集,在预训练模型上再训练,得到最终平均测试准确率为97.16%。相同试验条件下,该研究方法较支持向量机(Support Vector Machine,SVM)和BP(Back Propagation,BP)神经网络以及深度卷积模型(VGG-19和GoogLeNet Inception v2)分类效果更好。试验结果表明,通过迁移学习能把从源领域(PlantVillage数据集)学习到的知识迁移到目标领域(棉花病虫害数据集),数据增强技术能有效缓解过拟合。该研究为农作物病虫害识别技术的发展提供了参考。     

佳芦河流域水土保持监测及土壤侵蚀评价

以佳芦河流域分辨率为0.38 m的航摄影像和5 m的DEM等为信息源,基于ArcGIS平台,获取了流域水土保持措施、土地利用、植被覆盖度、坡度、沟壑烈度等土壤侵蚀影响因子,依据《土壤侵蚀分类分级标准》(SL 190—2007),对各因子进行叠加分析,对水蚀、风蚀区等不同侵蚀类型的土壤侵蚀强度进行了分析评价。结果表明,截至2012年9月,佳芦河流域有水土流失面积1068.89 km 2,占流域面积的94.26%,其中轻度、中度、强烈、极强烈、剧烈侵蚀面积分别为118.69、206.35、126.29、75.08、542.48 km 2;强烈及以上侵蚀面积占到水土流失面积的69.59%,其中强烈和极强烈侵蚀多发生在风蚀区,而剧烈侵蚀主要发生在水蚀区的沟道中。     

基于InVEST模型的祁连山国家级自然保护区土壤保持现状与功能

运用InVEST模型,对甘肃祁连山自然保护区土壤保持现状与功能进行了定量评估,分析了不同土地利用、海拔高度、坡度以及土壤类型下的保土状况。结果表明:2015年甘肃祁连山自然保护区土壤侵蚀量与土壤保持量分别为1. 67×10^8t、4.21×10^8t。从侵蚀面积来看,保护区以微度和轻度侵蚀为主,占总面积的63.95%;虽草地的土壤保持能力弱于其他自然植被类型,但草地是土壤保持总量最高的土地利用类型;不同海拔梯度下的土壤保持总量随海拔增加呈现先增后减的趋势,保护区内海拔2 500~3 500 m的土壤保持功能最好;栗钙土的土壤保持量最高,黑毡土在草原土壤类型中土壤保持强度较低;坡度为15°~25°的区域土壤保持量最大,占土壤保持总量的31.93%;甘肃祁连山保护区生态系统减少泥沙淤积和减少土地废弃的价值分别为5. 76×10^8元和1. 44×10^8元,保护区内林草地保肥价值为9. 03×10^10元。     

Evidence of sedimentation inequality along riparian areas colonised by Impatiens glandulifera (Himalayan balsam)

Soil loss from riparian areas supporting the annual invasive weed, Impatiens glandulifera (Himalayan balsam), was measured and compared with equivalent values recorded at nearby, topographically similar areas supporting perennial vegetation over a cumulative seven-year period, along sections of two separate river systems; one in Switzerland, and one in the UK. Soil loss from colonised locations was significantly greater than from reference locations in four of the seven measurement periods. Despite contrasting results, standard deviations, based on soil losses and gains, were predominantly higher for colonised areas at both rivers over most monitoring periods. These findings indicated that areas colonised by Himalayan balsam experience higher sediment flux in comparison with areas free of invasion. Here, we test those original interpretations by reinterrogating the datasets using a more robust analysis of inequality. Nine datasets were tested, five of which (i.e. 56%) showed that sediment flux was significantly greater at Himalayan balsam-invaded areas than at reference areas. Three datasets showed no difference in sediment flux between invaded and reference areas (33%), and one (11%) showed higher sediment flux at reference areas. Most results uphold our original interpretations and support our hypothesis that hydrochory probably dictates where colonisation initially occurs, by depositing Himalayan balsam seeds in slack or depressional areas along river margins. Once Himalayan balsam becomes established and sufficient perennial vegetation is displaced, seasonal die-off and depleted vegetation cover may increase the risk that some areas will experience significantly higher sediment flux.     

基于USLE模型的滹沱河上游黄土区土壤侵蚀空间特征研究

滹沱河是山西省面积较大的支流之一,研究滹沱河上游的土壤侵蚀对于建立山西省生态修复体系具有重要意义。以忻州市滹沱河上游为研究区,以遥感影像数据、数字高程模型数据、降雨数据、土壤类型数据为基础,利用GIS、RS技术,结合美国通用水土流失方程(USLE)估算滹沱河上游流域的土壤侵蚀模数。结果表明：（1）2015年滹沱河上游的土壤平均侵蚀模数为2538.9 t/(km ²·a),整体属于中等侵蚀水平。土壤侵蚀类型主要为微度侵蚀、极强烈和剧烈侵蚀;（2）随着高程海拔的升高,土壤侵蚀强度加大,土壤侵蚀面积减少,高程与土壤侵蚀强度呈正相关关系,与侵蚀面积呈负相关关系。剧烈侵蚀在各个高程带均有分布,在[500,1000)高程带中,微度侵蚀的面积范围最大;（3）研究区在0—5°带的土壤侵蚀面积分布最大;（4）牧草地的土壤侵蚀分布范围最广,其次分别为耕地>林地>园地>城镇村及工矿用地>水域及水利设施用地>其他土地。研究结论可为政府制定土壤侵蚀治理的技术方法、治理方案以及治理工程类型、规模及布局等提出科学依据。     

树轮地貌学方法在坡面土壤侵蚀调查中的应用——以河北省环首都山地为例

通过对树根解剖法的综合分析,提出了基于全树龄的坡面土壤侵蚀调查方法。利用该方法,选择河北省涞源县、兴隆县两地作为典型调查点,对河北省环首都山地的坡面土壤侵蚀进行了调查,探讨了树龄分析法在不同地貌部位、不同岩性、不同树种条件下土壤侵蚀研究的可行性。结果表明,利用全树龄分析方法所取得的坡面水土流失数据与RUSLE模型具有一定的可比性,而且基于全树龄的树轮地貌学方法对研究区土壤侵蚀情况的时空变化特征具有更强的指示性和分辨率,实用性更高。     

基于SHPB试验的桦木压缩动力学特性

【目的】利用木材动态压缩加载试验研究热磨机研磨解离破碎阶段木材原料受动态压缩载荷的动力学特性，并研究应变率、加载方向对木材原料动力学特性的影响，旨在深化木材原料研磨解离机制的研究，为热磨法纤维分离设备及磨片的齿形结构优化设计提供理论指导。【方法】利用 Hopkinson 杆试验装置对含水率为12.65%、密度为0.50 g·cm －3的桦木试件进行应变率约为400，800，1200 s －1，加载方向为径向、弦向和轴向的动态压缩试验，获得桦木在不同应变率及方向上动态压缩加载的解离特征、动态应力－应变曲线及相应的力学特性。【结果】对比分析各组试验后试件的破坏形态发现：1)当应变率约为400 s －1时，径向、弦向和轴向加载的试件主要发生塑性变形；2)当应变率约为800 s －1时，径向加载试件被解离成几大块，并且有一些“火柴棍”状的小试件从大试件上剥离；弦向加载试件沿加载方向上产生更大的塑性变形，并且在试件上、下两端处沿加载方向产生贯穿性裂纹，试件被解离成三大块；轴向加载试件受载面边缘处的纤维大量产生压溃现象，在加载面上产生贯穿性裂纹且有片状小试件从大试件上剥离；3)当应变率约为1200 s －1时，径向加载试件被解离成大量“火柴棍”状的小试件，并且小试件的尺寸明显小于应变率为800 s －1时；弦向加载试件沿加载方向上产生的塑性变形与应变率为800 s －1时相当，但是试件上端处被解离成许多片状的小试件，并且沿加载方向试件上产生了数条贯穿整个试件的大裂纹；轴向加载试件被解离成大量短粗状的小试件，并且小试件上带有明显的褶皱。对比分析各组试验试件的应力－应变曲线发现：1)动态压缩加载条件下桦木的应力－应变曲线可以由屈服点应变分为弹性阶段和屈服后弱线性强化阶段2部分；2)桦木沿径向加载应变率约为400，800，1200 s －1时，其屈服强度和韧性模量分别为4.56，10.49，14.22 MPa 和2.88，8.32，20.70 kJ·cm －3，应变率从400 s －1增加到1200 s －1时，屈服强度和韧性模量分别增加了2.11和6.19倍；3)桦木沿弦向加载应变率约为400，800，1200 s －1时，其屈服强度和韧性模量分别为5.87，7.90，9.65 MPa 和2.53，7.41，12.92 kJ·cm －3，应变率从400 s －1增加到1200 s －1时，其屈服强度和韧性模量分别增加了0.64和4.10倍；4)桦木沿轴向加载应变率约为400，800，1200 s －1时，其屈服强度分别为22.90，71.41，96.37 MPa 和18.79，67.74，114.32 kJ·cm －3，应变率从400 s －1增加到1200 s －1时，其屈服强度和韧性模量分别增加了3.21和5.08倍。【结论】随着应变率的增加，桦木的解离程度加大，径向加载最易解离，轴向加载最难解离；桦木的动态压缩屈服强度、动态压缩韧性模量具有很强的应变率敏感性，是一种应变率敏感材料。     

内蒙古京津风沙源治理工程土壤风蚀控制效益研究

2000—2013年内蒙古风沙源治理工程区风蚀模数整体呈现下降趋势,风蚀程度有所减轻。5个亚治理区风蚀模数差异较大,其中浑善达克沙地治理区风蚀模数最高,其他依次为科尔沁沙地南缘治理区﹥乌兰察布高平原退化草原、荒漠草原治理区﹥锡林郭勒高平原-乌珠穆沁沙地盆地退化草原治理区﹥华北北部丘陵山地水源涵养治理区。工程区土壤风蚀量明显减少,2001—2013年累计净减少1 370 446.65×104t,其中,乌兰察布高平原退化草原、荒漠草原治理区累计净减少风蚀量最大;其次为锡林郭勒高平原-乌珠穆沁沙地盆地退化草原治理区。风力是造成内蒙古风沙源工程区土壤侵蚀的最主要营力。2000—2013年,工程区风蚀模数与风蚀量的逐步降低说明,京津风沙源治理工程实施十余年以来,通过实施各类治理措施,工程区土壤风蚀得到初步控制,工程区生态状况趋向好转,随着森林资源总量与质量的提高,水土流失状况进一步改善,沙化土地治理初见成效。     

Estimation of Runoff,Peak Discharge and Sediment Load at the Event Scale in a Medium‐Size Mediterranean Watershed Using the Annagnps Model

In this paper, the Annualized Agricultural Non‐Point Source (AnnAGNPS) model has been used to estimate runoff, peak discharge and sediment load at the event scale in a Mediterranean watershed. The study area is the Carapelle torrent, Southern Italy (area = 506 km²), where continuous rainfall, streamflow and sediment load data are available. Nineteen flood events have been registered in the period 2007–2009 and were used for the application of the model. The aim of the paper is to evaluate the predictive accuracy of the model at the event scale, in a medium‐size watershed, given the specific conditions of the semi‐arid environments. A sensitivity analysis has been carried out to assign the correct parameterization: the mean normalized output variation of the most meaningful input parameters pointed out the influence of the curve number on runoff, peak discharge and sediment load predictions (values greater than 1); the MN Manning's roughness coefficient and K, C and P factors of the universal soil loss equation showed a moderate influence on sediment load simulations (values between 0·5 and 1). The selection of the Soil Conservation Service synthetic storm types has been based on the observed storm events analysis to improve the peak discharge simulations. The model prediction has proved to be good for runoff (R² = 0·74, NSE = 0·75, W = 0·92) and peak discharge (R² = 0·85, NSE = 0·70, W = 0·94), and satisfactory for sediment yield (R² = 0·70, NSE = 0·63, W = 0·91). The relative error is lower for high events; this result is quite interesting in semi‐arid environments, where most of the annual sediment yield is concentrated in a few, severe events. Copyright © 2013 John Wiley & Sons, Ltd.     

The role of shelter in Australia for protecting soils,plants and livestock

The purpose of this review is to examine the current knowledge of the role of trees in providing shelter for pastures, crops, and livestock, for controlling erosion of soils and improving productivity and sustainability of agricultural production in Australia — and the extent to which this knowledge has been applied.Land degradation — tree loss and associated soil salinity, water and wind erosion, soil acidification, soil structural decline and nutrient degradation — is evidence that our primary production systems are not sustainable. We have sought increased production without proper consideration of the ecological context of that system. About half of Victoria's crop and pasture lands are affected or at risk, and in Western Australia about 25% of the cleared agricultural land is wind-eroded and 60% is potentially susceptible, salinity affects 0.43 m ha and half of the divertible surface water is affected by salinity. Similar problems occur in other States. At least 43 m ha or 13% of our rangelands are seriously degraded by wind erosion caused by overgrazing, often coinciding with drought or a run of drier years.Minimum tillage and stubble management for erosion control in cropping has been a major extension and research activity in Australian agriculture. Severe weather, combined with imperfect adoption of appropriate grazing and crop management systems, shows the weakness of complete reliance on these methods of erosion control. An effective system must accommodate the impact of extreme events, which are the most damaging. However, the complementary use of windbreaks to reduce soil erosion is rare, and their establishment has not been promoted, despite the wide-spread adoption of this technology by other countries.In the cropping and higher rainfall grazing areas, the systematic planting of 10% of the land in a net of shelterbelts/timberbelts/clusters could achieve a 50% windspeed reduction; this would substantially improve livestock and pasture production in the short and long-term. Wind erosion could be dramatically reduced and crop production probably increased by the use of windbreaks. Wheat and oat yield at Rutherglen (Victoria), and lupin yield at Esperance (Western Australia), were increased in the sheltered zone by 22% and 47%, and 30%, respectively.In semi-arid and dry temperate areas, planting of 5% of the land to shelter could reduce windspeed by 30–50% and soil loss by up to 80%. This planting would also contribute substantially to achieving other objectives of sustainable agriculture. Agroforestry — particularly timberbelts applications — will be important in the long-term strategy for achieving revegetation. If some of the trees yield a marketable product then the adoption of the system will be more readily achieved.In the arid (pastoral) areas there is an urgent need to promote the ethic that preservation and improvement of the perennial grass and shrub vegetation is critical for the protection of the soil and maintenance of land capability. Control of animal grazing remains the sole means of preventing erosion in much of this zone. While satellite imagery allows us to assess the condition of leasehold lands, we have failed to achieve stocking policies that will halt the degradation of our rangelands.