Short time effects of biological and inter-row subsoiling on yield of potatoes grown on a loamy sand,and on soil penetration resistance,root growth and nitrogen uptake

Soil compaction, especially subsoil compaction, in agricultural fields has increased due to widespread use of heavy machines and intensification of vehicular traffic. Subsoil compaction changes the relative distribution of roots between soil layers and may restrict root development to the upper part of the soil profile, limiting water and mineral availability. This study investigated the direct effects of inter-row subsoiling, biological subsoiling and a combination of these two methods on soil penetration resistance, root length density, nitrogen uptake and yield. In field experiments with potatoes in 2013 and 2014, inter-row subsoiling (subsoiler) and biological subsoiling (preceding crops) were studied as two potential methods to reduce soil penetration resistance. Inter-row subsoiling was carried out post planting and the preceding crops were established one year, or in one case two years, prior to planting. Soil resistance was determined with a penetrometer three weeks after the potatoes were planted and root length density was measured after soil core sampling 2 months after emergence. Nitrogen uptake was determined in haulm (at haulm killing) and tubers (at harvest). Inter-row subsoiling had the greatest effect on soil penetration resistance, whereas biological subsoiling showed no effects. Root length density (RDL) in the combined treatment was higher than in the separate inter-row and biological subsoiling treatments and the control, whereas for the separate inter-row and biological subsoiling treatments, RLD was higher than in the control. Nitrogen uptake increased with inter-row subsoiling and was significantly higher than in the biological subsoiling and control treatments. However, in these experiments with a good supply of nutrients and water, no yield differences between any treatments were observed.     

土壤温度对作物根区环境及玉米根冠生长的调控研究进展

土壤温度对作物的生长发育具有很强的调控作用。在全球气候变化背景下,根区土壤温度对玉米生长的影响及其调控机制已成为当前研究的一个热点。结合目前农业生产中土壤低温和高温对玉米造成危害的现状,从土壤温度对作物根区土壤环境以及玉米根系生长、冠层发育与产量形成的影响方面,综述土壤温度对玉米生长发育调控作用的研究进展,介绍改变土壤温度的措施以及对玉米土壤温度研究的发展方向进行展望,为今后的研究提供参考。     

Greater humification of belowground than aboveground biomass carbon into particulate soil organic matter in no-till corn and soybean crops

Quantifying the amount of carbon (C) incorporated from decomposing residues into soil organic carbon (C_S) requires knowing the rate of C stabilization (humification rate) into different soil organic matter pools. However, the differential humification rates of C derived from belowground and aboveground biomass into C_S pools has been poorly quantified. We estimated the contribution of aboveground and belowground biomass to the formation of C_S in four agricultural treatments by measuring changes in δ¹³C natural abundance in particulate organic matter (C_POM) associated with manipulations of C₃ and C₄ biomass. The treatments were (1) continuous corn cropping (C₄ plant), (2) continuous soybean cropping (C₃), and two stubble exchange treatments (3 and 4) where the aboveground biomass left after the grain harvest was exchanged between corn and soybean plots, allowing the separation of aboveground and belowground C inputs to C_S based on the different δ¹³C signatures. After two growing seasons, C_POM was primarily derived from belowground C inputs, even though they represented only ∼10% of the total plant C inputs as residues. Belowground biomass contributed from 60% to almost 80% of the total new C present in the C_POM in the top 10 cm of soil. The humification rate of belowground C inputs into C_POM was 24% and 10%, while that of aboveground C inputs was only 0.5% and 1.0% for soybean and corn, respectively. Our results indicate that roots can play a disproportionately important role in the C_POM budget in soils. Keywords Particulate organic matter; root carbon inputs; carbon isotopes; humification rate; corn; soybean.     

茶树空中压条不定根原基发育影响因子研究

为了筛选出促使茶树茎段空中压条后发根的最佳技术方案,研究了成熟度、外施激素浓度、枝梢茎粗以及环割方式对根原基发育的影响.结果表明:选择生长健壮、茎粗为0.252 ～0.280 cm的当年生枝条,在黄绿色或青绿色茎段处进行传统环割,外用100 mg/L的ABT 1号生根粉处理,能有效缩短根原基发育周期.经过40～50 d...     

不同根颈直径苜蓿生理生化特性对低温胁迫的响应

为了探究不同颈粗苜蓿（Medicago sativa L.）的抗寒性与其根颈中生理生化特性的关系。以‘公农1号’紫花苜蓿为试验材料,对不同颈粗（3.50 mm,5.25 mm,7.00 mm）苜蓿根系进行低温胁迫（4℃,-10℃,-15℃,-20℃）处理,测定了苜蓿根颈活力、非结构碳氮含量和抗氧化酶活性。结果表明：低温胁迫对苜蓿根颈活力、非结构碳氮含量、非结构碳氮比（Cnstructured carbon nitrogen ratio,C/N）及过氧化氢酶（Catalase,CAT）活性均有极显著影响（P<0.01）;随低温胁迫的增加不同颈粗的苜蓿根颈活力均降低,可溶性糖和可溶性蛋白含量均呈增加-降低-增加的变化,淀粉含量、C/N和CAT活性均呈先增加后降低的趋势;苜蓿根颈活力大小与根颈中可溶性糖含量、可溶性蛋白含量、CAT活性及C/N显著相关（P<0.05）。研究认为,根颈直径大的苜蓿抗寒性较强,其通过调控根颈中可溶性蛋白、可溶性糖含量和CAT活性及C/N以适应低温胁迫。     

水分胁迫对紫花苜蓿根系吸水与光合特性的影响

变水条件下(利用PEG-6000模拟水分胁迫48 h,ψs=0.2MPa,之后复水48 h),测定紫花苜蓿(Medicago sattva L,品种阿尔冈金和陇东苜蓿)幼苗根系水力学导度与光合参数变化规律,旨在研究变水条件下紫花苜蓿光合作用的响应机制、植株水分吸收能力的变化规律及地上与地下部可能的相关关系.结果表明:干旱胁迫使得紫花苜蓿根系水力学导度(Lpr)受到显著影响.随着水分胁迫时间的延长,根系吸水能力呈现快速--缓慢下降趋势,即根系水力学导度逐渐下降,气孔导度(Gs)、蒸腾速率(Tr)、净光合速率(Pn)和叶片水势亦随之而显著降低,胞间二氧化碳浓度(Ci)先随之降低但最终上升而累积.复水后,根系水导呈现缓慢--慢速的恢复趋势,Pn、Gs、Tr、叶片水势随着根系水导速率的增加而逐渐恢复;Ci则随复水时间的延长而逐渐下降.但各参数除Ci外,均没有恢复到胁迫前水平.紫花苜蓿根系水导与光合参数在复水后的恢复程度说明,紫花苜蓿对干旱逆境的抵御与适应能力相对较弱,但陇东苜蓿对水分胁迫的忍耐能力强于阿尔冈金.     

退化高寒草甸斑块根—土复合体特征研究

高寒草甸斑块的根-土复合体对局部水土流失过程具有调控作用,为研究其特征及抗侵蚀效应,本研究选取三江源区达日县境内典型中度退化草甸的植被斑块为研究对象,调查草甸斑块中心与边缘植物群落特征,测定斑块边缘0～10 cm土层和斑块中心0～20 cm土层的容重、含水率、毛管孔隙度等土壤物理性质,并开展单根拉伸和根-土复合体直剪试验。结果表明：受优势种矮嵩草的分布影响,地上生物量主要分布在斑块中心,根系主要分布在0～10 cm土层;斑块中心区域土壤抗剪强度、内摩擦角和粘聚力均随土层深度的增加而减小;斑块边缘区域土壤粘聚力,抗剪强度明显高于斑块中心区域,草甸斑块植物根系是土壤抗剪强度的主要影响因素。草甸斑块根-土复合体能明显增加退化草甸土壤的抗侵蚀能力,研究结果可为深入研究高寒草甸根系固土功能及水土流失调控提供科学依据。     

穿龙薯蓣根的诱导和快繁及薯蓣皂苷元含量的测定

以穿龙薯蓣的丛生芽为材料,对根的诱导及快速繁殖进行了研究,并利用反相高效液相色谱技术对根中薯蓣皂苷元含量进行了测定,结果如下：不添加任何激素的1/2MS培养基是诱导生根的最佳培养基,生根率最高达76.7%;MS＋0.2 mg/L NAA＋0.5 mg/L IBA＋0.2-0.5 mg/L PP333为根增殖的最佳培养基,60 d时增殖倍数超过93;快繁过程中根的生长形态发生变化,不同类型的根中薯蓣皂苷元含量差异不显著,平均为0.21%     

GA3和PP333对萝卜生长及产量的影响

通过研究不同浓度的GA3和PP333及两激素不同浓度的互作对萝卜叶面积、叶重量、叶子叶绿素含量及根冠比的影响。结果表明，两者对叶子叶绿素含量没明显影响，但GA3在促进叶子的生长，叶面积的增大上以10~30ppm效果最好，而PP333虽然能抑制叶子的生长，但在肉质根生长中后期试用50ppm浓度的PP333，抑制了叶子的生长，反而促进了光合产物输送到肉质根，起到增产的作用。适当浓度的GA3和PP333及两者结合增产效果明显     

耕作土壤表面不平度分析

利用激光式不平度测试仪测定犁耕耕地地面、圆盘耙耙地地面和驱动耙耙地地面的不平度，测定地面不平度沿着3个方向进行，即平行、倾斜和垂直于耕作方向。对每一种地面不平度的RMS高度、自相关长度和自相关函数进行了分析，结果表明：对于短的地块，可用单一尺度来表征地表不平度的特征，地表不平度特征属于指数相关函数，RMS高度和自相关长度具有明显的相关性；对于长的地块，平整的农业地表不平度具有分形性或多尺度性，其自相关函数是一种分形过程。