大豆连作土壤肥力变化与有害生物发生的关系

1995—2003年采用定点定期采样系统调查与室内测定相结合的方法,针对连作大豆土壤营养含量、病虫基数与植株体营养,生物学性状、病虫草发生及产量品质的关系进行了研究,并对各相关性状间的关系进行了系统的统计分析,建立了数学模型,对指导大豆的高产优质栽培具有重要的意义。     

无细胞分裂素培养基上高效的大豆下胚轴外植体器官再生

虽然已经有大豆下胚轴再生植株的很多报道，但再生率总是很低并且不定芽的再生都是在添加细胞分裂素的培养基上取得的。这种培养基使外植体形成大量愈伤组织且阻碍了再生芽的进一步生长。为此本实验将表面灭菌的成熟种子置2种培养基上萌发，一种添加2 mg/L苄基腺嘌呤（BA）而另一种不添加；6 d后将小苗的下胚轴切下作为外植体培养到两种诱导不定芽再生的培养基上，同样一种添加2 mg/L BA而另一种不添加。在9个当地、2个美国和1个巴西共12个供试品系中，最好的培养结果是在含2 mg/L BA的培养基上萌发、长 苗、切取下胚轴并在不含BA的再生培养基诱导不定芽。以此程序，不定芽的再生率和质量都得到了显著提高，其中一个当地品种“广大粒”的再生率达到了72%。     

大豆水溶性多糖的黏度性质及其应用研究

研究了不同条件下大豆水溶性多糖溶液的黏度变化情况，同时和其他常用的稳定剂如果胶等也做了比较。试验结果表明。本实验室生产的大豆水溶性多糖的水溶液的黏度随着温度的升高、浓度的降低、外加盐量的增加而降低；随着外加蔗糖量、pH值的增加而增加；相比较于其他稳定剂大豆水溶性多糖的黏度很低，使酸乳饮料具有清爽的口味。     

大豆叶片性状和叶绿素含量QTL间的上位性和环境互作效应

以丰产性好、抗旱力强的栽培大豆晋豆23为母本,山西农家品种半野生大豆灰布支黑豆为父本杂交衍生的447个RIL作为供试群体。将亲本及447个家系分别于2011、2012和2013年采用随机试验种植,按照标准测量叶长、叶宽和叶柄长3个性状,并于2012年8月1日和8月8日和2013年8月2日和8月9日各测量1次叶绿素含量。采用QTLNETwork 2.0混合线性模型分析方法和主基因+多基因混合遗传分离分析法,对大豆叶片性状和叶绿素含量进行遗传分析和QTL间的上位性和环境互作效应研究。结果表明,叶长受2对加性-加性×加性上位性混合主基因控制,叶宽受3对等效主基因控制,叶柄长受4对加性-加性×加性上位性主基因控制,叶绿素含量受4对加性主基因控制;检测到10个与叶长、叶宽、叶柄长和叶绿素含量相关的QTL,分别位于A1、A2、C2、H_1、L和O染色体。其中2个叶长QTL分别位于C2和L染色体,是2对加性×加性上位互作效应及环境互作效应QTL;3个叶宽加性与环境互作QTL分别位于A2、C2和O染色体;2个叶柄长QTL分别位于L和O染色体;3个叶绿素含量QTL分别位于A1、C2和H_1染色体。叶片性状和叶绿素含量的遗传机制较复杂,加性效应、加性×加性上位互作效应及环境互作效应是大豆叶片性状和叶绿素含量的重要遗传基础。建议大豆分子标记辅助育种中,一方面要考虑起主要作用的QTL,另一方面要注重上位性QTL的影响,这对于性状的遗传和稳定表达具有积极的意义。     

大豆孢囊线虫4号生理小种侵染大豆根系诱导表达的cDNA分析

大豆孢囊线虫(Heterodera glycines Ichinohe；Soybean Cyst Nematode，SCN)是一种土传的专性内寄生线虫。SCN的二龄幼虫侵入到大豆幼嫩的根组织中，导致大豆根内的细胞变形并与之形成“合胞体”。合胞体在形态上和生理上的变化是SCN直接诱导大豆基因表达的结果。本研究以高抗SCN的灰布支黑豆为材料，用大豆孢囊线虫二龄幼虫直接接种大豆的根系，应用DDRT—PCR技术及RDB(Reversedot—blotting)杂交鉴定，获得6个阳性cDNA克隆，分别是SCN侵染后5天的A32克隆(GenBank登录号为B1173978)；侵染后10天的B12克隆(GenBank登录号为B1173979)、B71克隆(GenBank登录号为B1173980)；侵染后15天的Cll克隆(GenBank登录号为B1173981)、CPl2(GenBank登录号为B1173982)克隆和CP32克隆(GenBank登录号为B1173983)。序列的同源比较表明，6个cDNA均与Shoemaker构建的大豆基因表达库中的cDNA序列有非常高的同源性，证明这些cDNA是大豆基因表达的产物。其中A32克隆的序列与控制拟南芥下胚轴生长的MYB转录因子、营养元素缺失诱导的番茄根的表达文库中的一个cDNA及番茄抗假单胞杆菌表达文库中的一个cDNA有较高的同源性。     

Soil carbon and nitrogen changes as affected by tillage system and crop biomass in a corn–soybean rotation

A wide range of tillage systems have been used by producers in the Corn-Belt in the United States during the past decade due to their economic and environmental benefits. However, changes in soil organic carbon (SOC) and nitrogen (SON) and crop responses to these tillage systems are not well documented in a corn–soybean rotation. Two experiments were conducted to evaluate the effects of different tillage systems on SOC and SON, residue C and N inputs, and corn and soybean yields across Iowa. The first experiment consisted of no-tillage (NT) and chisel plow (CP) treatments, established in 1994 in Clarion–Nicollet–Webster (CNW), Galva–Primghar–Sac (GPS), Kenyon–Floyd–Clyde (KFC), Marshall (M), and Otley–Mahaska–Taintor (OMT) soil associations. The second experiment consisted of NT, strip-tillage (ST), CP, deep rip (DR), and moldboard plow (MP) treatments, established in 1998 in the CNW soil association. Both corn and soybean yields of NT were statistically comparable to those of CP treatment for each soil association in a corn–soybean rotation during the 7 years of tillage practices. The NT, ST, CP, and DR treatments produced similar corn and soybean yields as MP treatment in a corn–soybean rotation during the 3 years of tillage implementation of the second experiment. Significant increases in SOC of 17.3, 19.5, 6.1, and 19.3% with NT over CP treatment were observed at the top 15-cm soil depth in CNW, KFC, M, and OMT soil associations, respectively, except for the GPS soil association in a corn–soybean rotation at the end of 7 years. The NT and ST resulted in significant increases in SOC of 14.7 and 11.4%, respectively, compared with MP treatment after 3 years. Changes in SON due to tillage were similar to those observed with SOC in both experiments. The increases in SOC and SON in NT treatment were not attributed to the vertical stratification of organic C and N in the soil profile or annual C and N inputs from crop residue, but most likely due to the decrease in soil organic matter mineralization in wet and cold soil conditions. It was concluded that NT and ST are superior to CP and MP in increasing SOC and SON in the top 15 cm in the short-term. The adoption of NT or CP can be an effective strategy in increasing SOC and SON in the Corn-Belt soils without significant adverse impact on corn and soybean yields in a corn–soybean rotation.     

Multivariate effects of plant canopy, soil physico-chemistry and microbiology on Sclerotinia stem rot of soybean in relation to crop rotation and urban compost amendment

The effects of canopy, soil physico-chemical and microbiological variables on Sclerotinia stem rot (SSR) on soybean were assessed in two soils (clay loam and sandy loam) using multiple regression and canonical redundancy analysis (RDA) and their partial form to control for the rotation (2 or 3-y-corn/soybean monoculture) and fertilization (mineral/urban compost) or spatial variables effects. The models revealed the minimal sets of variables that best explain the variance of the survival of Sclerotinia sclerotiorum’s sclerotia, carpogenic germination, disease severity and their associations. In clay loam, the 3-y-corn rotation reduced disease severity mainly through the reduction of weed biomass that favoured carpogenic germination. Urban compost has a conducive effect explained by a better soil surface drainage. Additionally, total N was found suppressive to sclerotial survival. In sandy loam, the carpogenic germination was negatively correlated with high C mineralization quotient and aggregate stability but correlated positively with Ca. Sclerotial survival was negatively correlated with pH and Ca, and positively correlated with biological fertility index. Aggregate stability, Ca and pH were associated with the urban compost. The regression and RDA analyses allowed to identify key variables that drived SSR development and explain their relationship with the cultural practices, soil health, as well as the spatial variation of disease variables.     

The effect of growing soybean (Glycine max. L.) on N2O emission from soil

A pot experiment was conducted to investigate the effect of growing soybean on N₂O emission from soil. When soybean was growing in pots, the cumulative N₂O emission during the growing season was 2.26 mg N pot⁻¹, which was 5.9 times greater than that from the identical but unplanted pots (CK). However, the difference in N₂O fluxes between the two treatments was not significant until the grain-filling stage. Of the total N₂O emission, 94% took place during the period from grain-filling to ripening. Premature harvesting of the aerial parts of the plants at various growth stages substantially stimulated N₂O emission from the soil. These results implied that the process of symbiotic N fixation per se does not stimulate N₂O production or emission, but rather senescence and decomposition of the roots and nodules in the late growth stage. Therefore, additional N₂O would be emitted from the soil after harvesting of soybean with roots, litter, and residues left in situ.     

桑树大豆间作地上部和地下部的种间作用研究

在田间条件下研究了桑树-大豆间作体系中地上部分和地下部分之间的相互作用。结果表明:在桑树和大豆间作的共生期间,间作桑树地上部生物量、光合速率、含N量、根系干重、根长密度和叶片硝酸还原酶活性(NRA)比单作桑树分别增加了65.9%、11.8%、17.8%、24.8%、139.8%和116.2%,而大豆呈现相反趋势,桑树和大豆间作期间存在明显的竞争关系。但是,间作大豆土壤微生物生物量碳和土壤脱氢酶活性分别比单作大豆高10.6%和3.5%,桑树和大豆间作存在种间促进作用。因此,桑树和大豆间作体系中种间促进作用和种间竞争作用是同时存在的。     

吉林省大豆种植区土壤主要营养元素与大豆产量的相互关系研究

土壤中的营养元素是评价土壤自然肥力的主要因素之一。本文对吉林省大豆种植区土壤中的主要营养元素N、P、K的供应水平进行了分析 ,并探讨了它们与大豆产量之间关系。研究表明 :吉林省大豆种植区土壤供氮水平属于中级 ,供磷和供钾水平属于高级 ,并当土壤碱解氮 :有效磷 :有效钾接近 1∶0 .3～ 0 .4∶1.7～ 1.8时 ,大豆单产水平较高 ,为提高大豆单产、指导科学施肥提供了科学依据