基于PLSR-BP复合模型的红壤有机质含量反演研究

对红壤地区土壤有机质进行快速预测,以满足智慧农业与精准施肥的需要。以江西省奉新县北部为研究区域,采用1 km×1 km标准格网划分研究区进行采样,共得到红壤样本248个。对土壤光谱进行了包含分数阶导数在内的3种数学变换方法,将经过P=0.01显著性检验的波段用于模型的构建,选用偏最小二乘回归(PLSR)和BP神经网络建立土壤有机质含量预测模型。结果表明:当对红壤光谱数据进行1.5阶导数变换后再使用PLSR-BP复合模型对土壤有机质含量进行预测时的结果为最优,训练集R²=0.89,RMSE=4.68g·kg^-1,验证集R²=0.87,RMSE=5.55g·kg^-1,RPD=2.75。1.5阶导数对红壤光谱数据的变换能够更好地突出与有机质相关的特征信息,有助于其含量预测。PLSR-BP复合模型预测精度优于单一模型,能够较好地预测红壤有机质含量,为精准农业快速监测红壤有机质含量提供了新的途径。     

浅析现阶段农业有机废弃物利用存在的问题

简要分析利用有机废弃物的意义,提出我国现阶段农业有机废弃物利用方面存在的问题,并对相关解决途径提出建议。     

参与碳氮磷转化的水解酶对不同施肥响应的差异

本文旨在研究土壤水解酶对不同施肥的响应差异以及影响因素。通过在红壤中添加牛粪有机肥、化肥进行90d的室内土壤培养试验,采用微孔板荧光法动态分析5、30和90d参与碳氮磷转化的土壤水解酶(α-1,4-葡萄糖苷酶、β-1,4-葡萄糖苷酶、纤维素酶、木聚糖酶、亮氨酸氨基肽酶、β-1,4-N-乙酰氨基葡萄糖苷酶、磷酸酶)活性。与不施肥(对照)相比,在30 d后,化肥处理的总酶活性显著下降,对应的参与碳氮磷转化酶活性均有不同程度下降;而有机肥处理的总酶活性在培养期内均未发生显著变化,但是其α-1,4-葡萄糖苷酶显著增加,而磷酸酶活性显著降低。参与碳转化的4种水解酶中,只有α-1,4-葡萄糖苷酶活性对施肥的响应较强,且施加有机肥增加其活性而无机肥则降低其活性;对于参与氮转化的水解酶而言,化肥明显抑制了亮氨酸氨基肽酶活性,而有机肥增加了β-1,4-N-乙酰氨基葡萄糖苷酶活性;磷酸酶活性明显受到有机肥的抑制作用,而对化肥的响应总体不明显。不同水解酶对不同施肥的响应有明显差异,NMDS分析表明,α-1,4-葡萄糖苷酶和亮氨酸氨基肽酶响应最明显,其次为磷酸酶与木聚糖酶;相关和冗余分析显示,土壤p H、可溶...     

川西北高寒沙化草地围栏禁牧时段和恢复过程的耦合机理研究

川西北沙化草地在围栏禁牧生态恢复过程中,土壤中有机质、全氮、水解性氮变化特征,研究对象为:未修复沙化草地、围栏禁牧生态恢复时间分别为5年、10年的沙化草地,研究其不同围栏禁牧时间沙化草地0～40 cm土层土壤中有机质、全氮、水解性氮的变化.其结果表明,随着围栏禁牧时间的增长,各土层土壤有机质、全氮含量均增加,植被盖度、...     

烟草中非挥发性有机酸分析研究进展

综述了近50年来国内外烟草中非挥发性有机酸的分析研究进展,并对烟草中非挥发性有机酸的各种化学分析方法的局限性进行了比较,指出目前随着近红外光谱法在烟草中的不断应用,近红外光谱法能为烟草企业测定烟草中非挥发性有机酸提供一种快速、高效、简便的分析方法。     

3种低相对分子质量有机酸对土壤中DDT的解吸

选择不同质量浓度（3.4～2000 mg/L）的有机酸做土壤中的滴滴涕（DDT）解吸实验.结果表明：在质量浓度为3.4 mg/L时柠檬酸和苹果酸对土壤中DDT的解析率达到4.6%和3.5%,并且盐碱土中DDT的解析率要高于草甸土中的解析率.植物生长过程中根系会释放根系分泌物,这些根系分泌物会增加对土壤中有机污染物的净化,这是一种有长远利用价值的土壤净化方式.     

五大连池新生代火山泥有机成分检测及其指标相关性分析

[目的]探索五大连池火山泥生态,并为其演变规律提供数据支撑。[方法]以五大连池新生代火山泥为研究对象,利用改良熏蒸浸提法测定火山泥微生物碳、氮;利用化学滴定和比色法测定火山泥酶活性各指标,利用国标规定的土壤指标检测方法测定火山泥养分各指标。[结果]微生物量碳、氮分别以药泉山、火烧山火山泥带最高,5条泥带碳氮比均在10.00~13.00。过氧化氢酶、转化酶、脲酶、蛋白酶、纤维素酶含量分别以莫拉布山、火烧山、龙门山、火烧山、药泉山火山泥带最高,在研究区内,纤维素酶所占比重最大,脲酶最小,总酶含量以药泉山泥带最高。5条泥带全氮、全磷及全钾含量相对较均衡,分别在1.00~2.50、0.20~0.70、19.20~23.50 mg/g,分别以火烧山、龙门山、火烧山最高,有机质以火烧山含量最高。各有机成分间均呈现不同程度的相关性。[结论]药泉山和火烧山火山泥带各有机成分积累能力较强,矿化度较高。相关性分析表明,转化酶对环境变化的响应更为敏感。     

接种蚯蚓与添加有机物料对茶园土壤结构的影响

蚯蚓通过取食、排泄、分泌黏液、挖掘洞穴等活动,可显著改善土壤结构,提高土壤肥力.为探究蚯蚓与有机物料不同配施方式对茶园土壤肥力的调控效果与机理,设计5个处理组:不施肥(CK),不施肥+蚯蚓(BE),菜籽饼+蚯蚓(CE),茶树修剪物+蚯蚓(JE),生物质炭+蚯蚓(TE),分别进行室内模拟实验.结果显示,与不施肥(CK)相...     

Organic chlorine and chloride in submerged paddy soil: a case study in Anhui province, southeast China

Abstract. Efforts to understand the fate of organochlorine compounds in arable soil have concentrated on anthropogenic compounds, in spite of the fact that organochlorine compounds are both produced and mineralized in soil through natural processes. In order to understand the fate of chlorinated pesticides, it is necessary to take account of the natural chlorine cycle. The present study is a first attempt to illuminate the relationship between the natural chlorine cycle and agricultural practices. The concentration and storage of organic chlorine (Cl_org) and chloride (Cl_inorg) were determined in topsoil of a paddy field compared to an adjacent afforested hill at a sampling site in the Meicun area, Anhui Province, China. The concentration of Cl_org, as well as the chlorine-to-carbon ratio, was significantly lower in the paddy field samples than in the forest soil samples. A weak relationship between the concentration of Cl_org and the organic carbon content was observed in the paddy field, in contrast to the observations made in the adjacent forest soil as well as those made in previous studies, which have suggested a positive correlation between organic carbon content and Cl_org. The similarity between our results at the forest site and the previous studies, which have been carried out in temperate regions, suggests that it is the land use rather than the climate that makes the current paddy soil results different. Our results suggest that the contribution of Cl_org to the paddy soil from above-ground litter and from production within the soil are small or negligible compared with the contribution from pesticide application and wet and dry deposition.     

Potential chemical time bombs in the schelde estuary

The Schelde estuary is heavily polluted with many different (micro)pollutants. This results in high concentrations in the abiotic and biotic compartments of the Schelde estuary and in various effects. the present day suboxic and anoxic conditions in the upper estuary are probably responsible for the high distribution coefficients for some trace metals in the lower Schelde estuary (Western Schelde). a future reduction in discharges with a high biological oxygen demand will therefore not only result in higher oxygen concentrations, but probably also in lower distribution coefficients for trace metals in the Western Schelde. Simulations show that lower trace metal distribution coefficients will probably result in higher concentrations of dissolved (bioavailable) trace metals, even with substantially reduced discharge rates, due to the desorption of trace metals from resuspended bottom sediments.