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南方土壤中导致大豆皱叶的因子分析OA北大核心CSTPCD

Analysis of Factors Causing Soybean Crinkle Leaf in Southern China Soil

中文摘要英文摘要

为找出南方大豆皱叶症发生的诱因,本研究从南方土壤中非生物因素和生物因素两个角度进行探索研究.利用混池法和ICP-OES技术研究正常叶混池和皱叶混池的差异元素,利用构建的皱叶残留异质系中皱叶家系材料GY_C和正常叶家系材料GY_N,采用单因素随机区组试验设计,研究皱叶土壤的不同土层、营养液、灰烬、叶浆,进行土壤浸泡液、土壤消毒、氮肥等处理后大豆皱叶材料皱叶症的变化.结果表明:皱叶环境土壤的表层、中层和底层土均可导致GY_C叶片皱缩,中层土中的GY_C叶片皱缩程度略高于表层和底层土.氮磷钾配比失衡的营养液处理GY_C叶片未发生皱缩.ICP-OES分析皱叶混池E1和正常叶混池E0的31种元素后,未发现E1/E0比值为1.7倍以上的元素,且E1中锰元素含量低于E0.皱叶灰烬及土壤浸泡液处理基质后GY_C叶片未发生皱缩.移栽试验表明,南方土壤和基质比例超过3∶1时GY_C长出的新叶依然皱缩,而复种的盆栽中南方土壤和基质比例低于1∶8时GY_C叶片也会发生皱缩,且随着复种次数增加,皱叶程度有所增加.解剖观察皱叶材料的根、茎、叶柄未发现明显的虫害痕迹.-80,60,80,100和120℃处理的南方土壤中GY_C叶片不发生皱缩.综上所述,南方土壤中的微生物因素可能是导致大豆皱叶的关键因子.

To identify the causes of soybean leaf wrinkling in southern China,this study explored and studied from two perspectives:Non biological and biological factors in the soil of southern China.Differential mixing pool method and ICP-OES analysis technology was used to study the differential elements between the normal leaves mixing pool(Eo)and crinkle leaves mixing pool(E1).Two materials GY_C(crinkle grade is HS)and GY_N(crinkle grade is HR)with almost the same genetic background were used to study the change of soybean leaf wrinkling in different soil layers,nutrient solution,ash,leaf pulp,after soil soaking solution,soil disinfection,nitrogen fertilizer and other treatments.And random block test design was used in these experiments.The results showed that leaves of GY_C grown in surface,middle and subsurface layers soil all could cause the GY_C leaves becoming wrinkled.GY_C leaves grown in middle layers soil were more wrinkled than other two kind layers soil.GY_C leaves treated with nutrient solution in which the nitrogen phosphorus potassium ratio was imbalanced did not become wrinkled.ICP-OES analysis results showed that the value of E0/E1 to all elements were within 1.7-fold.And the manganese element content in E,was lower than that in E0.GY_C leaves did not collapse after treatment of the substrate with leaf ash and soil soaking solution.The transplanting experiment showed that the new leaves of GY_C continued to shrink when the southern soil and substrate ratio was more than 3:1,whereas the GY_C leaf also collapsed when the southern soil and substrate ratio was less than 1:8 in the pot with re-planting,and the degree of leaf shrinkage increased as the number of re-plications increased.Dissection and observation of the root,stem,and petiole of the crumpled leaf material revealed no obvious traces of infestation.The E1 soil treated under-80,60,80,100 and 120 ℃ could not cause GY_C leaves wrinkled.In summary,microbial factors in the southern soil may be the key factors that cause the crinkling of soybean leaves in southern China.

陈文杰;陈渊;韦清源;汤复跃;郭小红;梁江

广西农业科学院 经济作物研究所/广西作物遗传改良重点实验室,广西南宁 530007

大豆皱叶因子土壤南方ICP-OES

soybeancrinkle leaffactorsoilsouthern ChinaICP-OES

《大豆科学》 2024 (002)

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国家自然科学基金(32260451,32060490);广西自然科学基金(2019GXNSFAA185009);广西农业科学院稳定资助科研团队项目(2021YT055);现代农业产业技术体系建设专项(CARS-04-CES30).

10.11861/j.issn.1000-9841.2024.02.0167

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