Population dynamics of Macrophomina phaseolina in relation to disease management: A review

Macrophomina phaseolina (Tassi) Goid. causes seedling blight, charcoal rot, leaf blight, stem and pod rot on over 500 plant species in different parts of the world. The pathogen survives as sclerotia formed in host tissues which are released into the soil as tissue decay. Low soil moisture is considered the more important predisposing factor for M. phaseolina-induced diseases than high temperature. The intensity of the disease on a crop is related to the population of viable sclerotia in the soil and abiotic factors. The influence of various management strategies in reducing the number of viable propagules of the pathogen in the soil has been studied in order to minimize the impact of the disease. Any management approach that reduces inoculum density in the soil may reduce disease incidence on the host. However, to reduce inoculum density, quantitative determination of viable propagules from soil is necessary in order to understand the effect of management strategies on the population dynamics of this pathogen. Considerable work has been done on organic amendments, changing crop sequences with tolerant crops, fumigants, herbicides and tillage in managing M. phaseolina populations in the soil and the resulting disease. Solarization has been used in controlling M. phaseolina in different countries where this pathogen is causing disease on economically valuable crops. However, this method of soil disinfestation was effective in eliminating viable populations at the top soil layer although by combining other approaches its effectiveness was improved at lower soil depth. Use of biological control agents with or without organic amendments or after solarization has emerged to be a practical management approach in the control of M. phaseolina. In this paper, an attempt has been made to review those research findings where the influence of various management approaches on survival of M. phaseolina mainly sclerotia have been investigated.     

Comparison of phosphorus distribution and cycling between adjacent native semidesert shrub and cultivated grass-dominated ecosystems

Summary P concentrations at several soil profile depths and for various plant parts were monitored over most of one year in adjacent native semidesert shrub and cultivated crested wheatgrass ecosystems. When multiplied by appropriate soil bulk densities and phytomass values, it was possible to calculate P mineralomasses in these two ecotessera. Knowledge of new to old growth ratios allowed estimation of P turnover. Although there was greater P in the vegetation of the native stand, the tissues lived longer and decomposed less rapidly than those in the grass stand that has been established in a portion of the original shrub dominated semidesert. The grass stand showed higher net primary productivity and had a much higher fraction of phytomass that is consumable by livestock. There was thus, at least a five-fold greater turnover of P in the tilled and seeded system. The introduced grasses are also withdrewing more P from the soil reserves. Whether nutrient export from the systems could lead to long-term declines in productivity will require further monitoring and experimental effort.     

Identification of soil quality indicators for assessing the effect of different tillage practices through a soil quality index in a semi-arid environment

Tillage is known to potentially affect soil quality in various ways. In this study, a soil quality index (SQI) was developed by quantifying several soil attributes either sensitive or insensitive to physical disturbance, using factor analysis as a dimension reduction technique, in order to discriminate different tillage systems. Soil properties including physical (MWD), chemical (pH, organic C, total N, available P and POM contents) and microbial (MBC, MBN, PCM, PNM and three enzymes) parameters were measured to establish a minimum data set (MDS) for the assessment of overall SQI. The soil attributes were determined on samples (0–20 cm depth) collected under moldboard (MP) and disk (DP) plows as conventional tillage (CT), and rotary (RP) and chisel (CP) plows as reduced tillage (RT) systems with a similar plant C input rate and cover crop over a period of six years (2005–2011) in a semi-arid calcareous soil (Calcixerepts) from Central Iran. Results indicated a clear difference in soil quality among the tillage systems with a significant increase of SQI under RT over time, particularly under CP practices. Although RT improved most soil microbial attributes, not all attributes contributed to SQI because of their close interrelationship. The final SQI consisted only of geometric mean of microbial activity (GMA, the square root of the product of PCM and PNM) and geometric mean of enzyme activity (GME, the cube root of the product of enzyme activities). Soil GME and GMA were found to be as key indicators contributing 55% and 36% to SQI, respectively. Therefore, the GME and GMA were the most important indicators effectively discriminating tillage systems, and could be used to monitor the enhancement of soil quality under RT in this semiarid environment. The influence of tillage year on SQI was greater than that of tillage practices. In conclusion, RT systems were characterized by a higher value of SQI, suggesting a good recovery of soil capacity and functions after abandoning CT in the studied area. Smallholder farmers should therefore be aware of the potential for high soil quality in future as a result of continuing RT systems, especially with surface tillage using CP practices.     

残茬覆盖与耕作方式对夏玉米叶片衰老代谢和籽粒产量的影响

对小麦机械收获后残茬覆盖与不覆盖两种条件下免耕、翻耕和播种行深松3种土壤耕作方式的夏玉米开花后叶片衰老生理特性和籽粒产量进行了研究。结果表明,残茬覆盖和深松耕作的玉米叶片SOD和POD活性提高、MAD含量降低、叶绿素和可溶性蛋白质含量高、降解速度慢,维持了叶片后期较高的生理功能。最终开花后干物质生产量和玉米籽粒产量表现为：覆盖显著高于不覆盖,深松显著高于翻耕和免耕,残茬覆盖与深松结合效果最好。     

Spatial and Temporal Variation of Roots, Arbuscular Mycorrhizal Fungi, and Plant and Soil Nutrients in a Mature Pinot Noir (Vitis vinifera L.) Vineyard in Oregon, USA

Soil and crop management practices may influence biomass growth and yields of cotton (Gossypium hirsutum L.) and sorghum (Sorghum bicolorL.) and sequester significant amount of atmospheric CO₂in plant biomass and underlying soil, thereby helping to mitigate the undesirable effects of global warming. This study examined the effects of three tillage practices [no-till (NT), strip till (ST), and chisel till (CT)], four cover crops [legume (hairy vetch) (Vicia villosa roth), nonlegume (rye) (Secale cerealeL), hairy vetch/rye mixture, and winter weeds orno covercrop], and three N fertilization rates (0, 60–65, and 120–130 kg N ha ^–1) on the amount of C sequestered in cotton lint (lint + seed), sorghum grain, their stalks (stems + leaves) and roots, and underlying soil from 2000 to 2002 in central Georgia, USA. A field experiment was conducted on a Dothan sandy loam (fine-loamy, kaolinitic, thermic, Plinthic Kandiudults). In 2000, C accumulation in cotton lint was greater in NT with rye or vetch/rye mixture but in stalks, it was greater in ST with vetch or vetch/rye mixture than in CT with or without cover crops. Similarly, C accumulation in lint was greater in NT with 60 kg N ha ^–1 but in stalks, it was greater in ST with 60 and 120 kg N ha ^–1 than in CT with 0 kg N ha ^–1. In 2001, C accumulation in sorghum grains and stalks was greater in vetch and vetch/rye mixture with or without N rate than in rye without N rate. In 2002, C accumulation in cotton lint was greater in CT with or without N rate but in stalks, it was greater in ST with 60 and 120 kg N ha ^–1 than in NT with or without N rate. Total C accumulation in the above- and belowground biomass in cotton ranged from 1.7 to 5.6 Mg ha ^–1 and in sorghum ranged from 3.4 to 7.2 Mg ha ^–1. Carbon accumulation in cotton and sorghum roots ranged from 1 to 14% of the total C accumulation in above- and belowground biomass. In NT, soil organic C at 0–10 cm depth was greater in vetch with 0 kg N ha ^–1 or in vetch/rye with 120–130 kg N ha ^–1 than in weeds with 0 and 60 kg N ha ^–1 but at 10–30 cm, it was greater in rye with 120–130 kg N ha ^–1 than in weeds with or without rate. In ST, soil organic C at 0–10 cm was greater in rye with 120–130 kg N ha ^–1 than in rye, vetch, vetch/rye and weeds with 0 and 60 kg N ha ^–1. Soil organic C at 0–10 and 10–30 cm was also greater in NT and ST than in CT. Since 5 to 24% of C accumulation in lint and grain were harvested, C sequestered in cotton and sorghum stalks and roots can be significant in the terrestrial ecosystem and can significantly increase C storage in the soil if these residues are left after lint or grain harvest, thereby helping to mitigate the effects of global warming. Conservation tillage, such as ST, with hairy vetch/rye mixture cover crops and 60–65 kg N ha ^–1 can sustain C accumulation in cotton lint and sorghum grain and increase C storage in the surface soil due to increased C input from crop residues and their reduced incorporation into the soil compared with conventional tillage, such as CT, with no cover crop and N fertilization, thereby maintaining crop yields, improving soil quality, and reducing erosion.     

耕作方式对东北雨养区玉米光合与叶绿素荧光特性的影响

在东北地区设置大田试验,研究不同耕作方式下玉米全生育期耕层土壤温度、土壤含水量、叶片光合性能及叶绿素荧光参数的变化特征.结果表明:耕作方式对土壤水热性能的影响主要体现在播种-拔节阶段,2010-2011年平地播种中耕起垄(PL)和全生育期平作(PP)处理0～40 em土层土壤体积含水量在出苗期、苗期和拔节期比传统垄作(LL)处理平均提高5.6％和5.2％、4.6％和7.3％及3.9％和4.8％,苗期5 cm土壤最低温度分别比LL处理高1.4和1.3℃.由于土壤水热条件的改善,拔节期PL和PP处理的叶片净光合速率(Pn)、蒸腾速率(Tr)等指标显著高于LL处理,而PSⅡ潜在活性(Fv/Fo)和PSⅡ最大光化学效率(Fv/Fm)无显著差异,表明气孔导度和气孔限制值等气孔因素是导致光合作用差异的主要原因;灌浆期叶片Pn和Tr则以LL和PL处理显著高于PP处理,这主要是由于PP处理在强降雨时期经历了涝渍灾害,光合作用受到抑制.可见PL处理通过改善土壤水热条件增强了玉米光合性能,进而提高了籽粒产量.     

保护性耕作对农田碳、氮效应的影响研究进展

作物产量的高低主要取决于土壤肥力,如何保持并提高土壤肥力是确保我国粮食安全和农业可持续发展的重要任务,也是众多学者关注的焦点。土壤有机碳和氮素是评价土壤质量的重要指标,其动态平衡直接影响土壤肥力和作物产量。随着全球气候变化及环境污染问题的愈加突出,农田土壤固碳及提高氮效率成为各界科学家研究的热点。目前,保护性耕作已成为发展可持续农业的重要技术之一,对土壤固碳及氮素的利用具有很大的影响。深入了解保护性耕作对土壤有机碳固持与氮素利用效率提高的影响机制,对于正确评价土壤肥力有着重要意义。但由于气候、土壤及种植制度等条件不一致,关于保护性耕作对农田碳、氮效应结论不一。阐述了国际上保护性耕作对农田系统土壤有机碳含量变化及其分解排放(如CO₂和CH₄)、氮素变化及其矿化损失(如NH₃挥发、N₂O排放与氮淋失)和碳氮素相互关系(如C/N层化率)影响的研究进展,并分析了其影响因素和相关机理。尽管国内保护性耕作的研究已进行30 多年,但在土壤有机碳与氮素方面与国外相比依然有较大的差距。保护性耕作对土壤固碳与氮素利用的影响机制,碳素和氮素在土壤-植株-大气系统中的转移变化,及结合农事管理等综合评价其生态效应的研究很少。在此基础上,提出未来我国保护性耕作在土壤有机碳固定和氮素利用方面的重点研究方向:(1)在定位试验基础上进一步探讨保护性耕作对土壤有机碳及氮素利用的影响机制;(2)深入研究土壤有机碳和氮素的相互关系及其对土壤肥力的影响;(3)结合环境保护与土壤可持续管理对保护性耕作农田土壤固碳及氮素高效利用的系统评价研究;(4)加强保护性耕作对农田碳、氮效应的宏观研究,合理评价保护性耕措施下对农田碳、氮综合效应。     

耕作措施对土壤水热特性和微生物生物量碳的影响

通过山西寿阳设置的8a田间定位试验,比较了全量秸秆还田、免耕覆盖和常规耕作3种耕作措施下土壤含水量、温度及土壤微生物生物量碳变化.结果表明:免耕覆盖与全量还田处理显著提高土壤含水量,与常规耕作相比表层土壤体积含水量在玉米苗期、拔节期、灌浆期和成熟期分别高出18％、22％、29％、21％和3％、10％、12％、13％,具有保水保墒的作用.在苗期不同耕作措施对土壤温度的影响达到显著水平,5 cm处免耕覆盖、全量还田与常规耕作处理土壤温度依次为:18.12、18.76和19.44℃,免耕覆盖和全量还田处理平均温度比常规耕作分别低1.32℃和0.69℃.土壤微生物量碳在整个生育期动态变化是首先迅速上升在玉米生育高峰期(拔节期)达到最高峰,然后开始下降,成熟期趋于平缓.免耕覆盖与全量还田处理下玉米各生育期土壤表层微生物量碳显著高于常规耕作,在苗期、拔节期、灌浆期和成熟期分别比常规耕作高出70％、40％、85％和30％和10％、20％、15％和15％.土壤微生物量碳与土壤温度和土壤含水量相关和极相关.     

干热河谷石漠化区火龙果地不同耕作方式的土壤矿质元素特征

为探讨不同耕作方式的土壤矿质元素含量变化特征,促进火龙果生长发育和品质改良,该研究采用套种紫花苜蓿(Medicago sativa)、施用有机肥和化肥与农药、地膜覆盖和无措施五种耕作方式,以每种方式土壤的22种矿质元素为评价指标,比较不同耕作方式的矿质元素含量差异,阐明土壤矿质元素之间的相关关系。结果表明:(1)与无措施相比,其他耕作方式的Ca、Si、Mn等元素含量呈增加趋势,Fe、Mg、Al等元素含量则降低,Na含量无显著差异。(2)施用有机肥的矿质元素含量最丰富,地膜覆盖次之,套种紫花苜蓿最低。(3)相关性分析表明,火龙果地土壤矿质元素间多存在显著相关性,Al、Si、S、Ni与其他元素的相关性较密切,其次为Fe、Mg、Na、Mn、Cu和Co,均达到显著或极显著水平。(4) Ca、Fe、Mg、Mn、Cu、Zn和B之间多呈负相关,存在拮抗效应。干热河谷石漠化区在火龙果栽培时,应首选有机肥作为养分添加方式,并及时补充不同耕作方式造成的土壤矿质养分亏缺,尤其是Fe、Mg、Al、Na、Cu、Zn等元素。