Temporal and spatial patterns of soil water extraction and drought resistance among genotypes of a perennial C-4 grass

The objective of this study was to investigate patterns of soil water extraction and drought resistance among genotypes of bermudagrass (Cynodon spp.) a perennial C-4 grass. Four wild Australian ecotypes (1-1, 25a1, 40-1, and 81-1) and four cultivars (CT2, Grand Prix, Legend, and Wintergreen) were examined in field experiments with rainfall excluded to monitor soil water extraction at 30-190 cm depths. In the study we defined drought resistance as the ability to maintain green canopy cover under drought. The most drought resistant genotypes (40-1 and 25a1) maintained more green cover (55-85% vs 5-10%) during water deficit and extracted more soil water (120-160 mm vs 77-107 mm) than drought sensitive genotypes, especially at depths from 50 to 110 cm, though all genotypes extracted water to 190 cm. The maintenance of green cover and higher soil water extraction were associated with higher stomatal conductance, photosynthetic rate and relative water content. For all genotypes, the pattern of water use as a percentage of total water use was similar across depth and time We propose the observed genetic variation was related to different root characteristics (root length density, hydraulic conductivity, root activity) although shoot sensitivity to drying soil cannot be ruled out.

镧与钙的关系及对根系生理的影响

本研究通过探讨毛乌素沙地主要早生植物和中生植物的水分关系。对“早生植物”的概念作了进一步的分析的阐述，探讨了蒸腾作用、光合作用的气乳调节与植物叶片水分平衡的相互关系，并提出了以蒸腾“午体”为基础的关于划分植物水分生态类型的新概念。上述问题的探讨可作为对中国毛鸟素沙化化草地植物环境系统优化模式的水平衡假说的难证。探讨了为合理确定在研究地区种草造林的最佳密度所需进一步研究的内容：水分亏缺对植物量累积的抑制作用。并对该地区主要植物种的季节蒸腾耗水量作了估算。研究了依赖于主导环境因子的沙生植物蒸腾速率的回归模型。得出结论认为：对于蒸腾速率和叶面积指数，建立多元非线性回归可以取得较好结果。最后，对几个重要的蒸散预测模型和土壤水分运动的物理模型进行了评述，并探讨了这些模型对于干旱区蒸散预测研究的可行性，作为本研究的未来探讨的课题。

低分子有机酸对辣椒生长发育及叶片活性氧代谢的影响

采用盆栽试验与室内分析相结合的方法,研究了6种低分子有机酸和一种有机酸盐对辣椒生长发育和叶片活性氧代谢的影响。结果表明:柠檬酸、乙酰丙酸和有机酸钾处理不仅可显著提高辣椒根系干质量,增加辣椒vC含量,而且提高了辣椒的产量。甲酸、柠檬酸、乙酰丙酸和有机酸钾处理使根系活力比对照分别提高83%、93.8%、96.75%和99.5%。柠檬酸、乙酰丙酸和有机酸钾处理提高了辣椒叶片的SOD和POD活性,降低了膜脂过氧化产物MDA含量,延缓了叶片衰老。但是低分子有机酸处理对CAT活性的影响较小。

玉米根系活力杂种优势及其与光合特性的关系

对大田不同水分处理条件下玉米杂交种及其亲本在经济产量形成期的根系活力及其衰退的杂种优势进行了研究,并分析了根系活力与叶片光合特性之间的关系。结果表明,水分亏缺显著降低了玉米的根系活力;充分供水和水分亏缺条件下,玉米杂交种根系活力都具有显著的杂种优势;杂交玉米种根系活力衰退速率具有显著的负优势,抽雄后灌水能够显著降低玉米根系活力衰退速率。杂交玉米种在抽雄期各水分处理下的光合速率显著大于亲本;玉米根系活力与光合速率之间具有显著的正相关关系,随着根系活力的增高,玉米光合速率、气孔导度和蒸腾速率均增高。因此,杂交种较高的抗旱性是根冠共同作用的结果。在玉米育种和栽培中,要充分地考虑到根系对地上部生理活性的影响。

Atividade radicular da soja: definição de um método

Fundação de Amparo à Pesquisa do Estado de São Paulo (FAPESP)

Crescimento e atividade de raízes de soja em função do sistema de produção

O objetivo deste trabalho foi determinar o efeito de culturas de inverno e de primavera no crecimento do sistema radicular e na produtividade da soja, e comparar um método direto (trado) com um indireto (com rubídio), na análise do sistema radicular. Utilizou-se o delineamento experimental de blocos ao acaso, em parcelas subdivididas, com quatro repetições. As parcelas foram constituídas pelas culturas de inverno, triticale (X Triticosecale) e girassol (Helianthus annuus), e as subparcelas pelos culturas de primavera, milheto (Pennisetum glaucum), sorgo forrageiro (Sorghum bicolor) e crotalária júncea (Crotalaria juncea), além da escarificação, realizada em 2003 e 2009. A soja (Glycine max) foi cultivada no verão e seu sistema radicular foi avaliado por amostragem física das raízes, com trado, e por avaliação da atividade radicular com rubídio. Modificações na arquitetura ou na atividade do sistema radicular da soja não afetaram a produtividade. A distribuição física e a atividade radicular não foram afetados significativamente pelas espécies de inverno, mas o crescimento foi favorecido após o cultivo do milheto e do sorgo forrageiro, na primavera. A medida direta do sistema radicular com trado apresenta baixa correlação com a atividade radicular.

Avaliação do sistema radicular da soja sob sistemas de manejo do solo

Coordenação de Aperfeiçoamento de Pessoal de Nível Superior (CAPES)

Ciclagem de nutrientes em sistemas de rotação de culturas

Fundação de Amparo à Pesquisa do Estado de São Paulo (FAPESP)

Soil carbon balance in a tropical grassland: Estimation of soil respiration and its partitioning using a semi-empirical model

In savannah and tropical grasslands, which account for 60% of grasslands worldwide, a large share of ecosystem carbon is located below ground due to high root:shoot ratios. Temporal variations in soil CO2 efflux (R-S) were investigated in a grassland of coastal Congo over two years. The objectives were (1) to identify the main factors controlling seasonal variations in R-S and (2) to develop a semi-empirical model describing R-S and including a heterotrophic component (R-H) and an autotrophic component (R-A). Plant above-ground activity was found to exert strong control over soil respiration since 71% of seasonal R-S variability was explained by the quantity of photosynthetically active radiation absorbed (APAR) by the grass canopy. We tested an additive model including a parameter enabling R-S partitioning into R-A and R-H. Assumptions underlying this model were that R-A mainly depended on the amount of photosynthates allocated below ground and that microbial and root activity was mostly controlled by soil temperature and soil moisture. The model provided a reasonably good prediction of seasonal variations in R-S (R-2 = 0.85) which varied between 5.4 mu mol m(-2) s(-1) in the wet season and 0.9 mu mol m(-2) s(-1) at the end of the dry season. The model was subsequently used to obtain annual estimates of R-S, R-A and R-H. In accordance with results reported for other tropical grasslands, we estimated that R-H accounted for 44% of R-S, which represented a flux similar to the amount of carbon brought annually to the soil from below-ground litter production. Overall, this study opens up prospects for simulating the carbon budget of tropical grasslands on a large scale using remotely sensed data. (C) 2012 Elsevier B.V. All rights reserved.

Physiological and Biochemical Aspects of Iron Nutrition in Grapevine

The objective of this thesis was to study the response mechanisms of grapevine to Fe-deficiency and to potential Fe chlorosis prevention strategies. The results show that the presence of bicarbonate in the nutrient solution shifted the activity of PEPC and TCA cycle enzymes and the accumulation/translocation of organic acids in roots of Fe-deprived plants. The rootstock 140 Ruggeri displayed a typical behavior of calcicole plants under bicarbonate stress. The Fe chlorosis susceptible rootstock 101-14 reacted to a prolonged Fe-deficiency reducing the root activity of PEPC and MDH. Noteworthy, it accumulates high levels of citric acid in roots, indicating a low capacity to utilizing, transporting and/or exudating organic acids into the rhizosfere. In contrast, 110 Richter rootstock is capable to maintain an active metabolism of organic acids in roots, accumulating them to a lesser extent than 101-14. Similarly to 101-14, SO4 genotype displays a strong decrease of mechanisms associated to Fe chlorosis tolerance (PEPC and MDH enzymes). Nevertheless it is able to avoid excessive accumulation of citric acid in roots, similar as 110 Richter rootstock. Intercropping with Festuca rubra increased leaf chlorophyll content and net photosynthesis. In addition, intercropping reduces the activity of PEPC in roots, similary to Fe-chelate supply. Applications of NH4+ with nitrification inhibitor prevents efficiently Fe-deficiency, increases chlorophyll content, and induces similar root biochemical responses as Fe-EDDHA. Without the addition of nitrification inhibitors, the effectiveness of NH4+ supply on Fe chlorosis prevention resulted significantly lower. The aspects intertwined in this investigation highlight the complexity of Fe physiology and the fine metabolic tuning of grapevine genotypes to Fe availability and soil-related environmental factors. The experimental evidences reveal the need to carry out future researches on Fe nutrition maintaining a continous flow of knowledge between theoretical and agronomical perspectives for fully supporting the efforts devoted to convert science into practice.

Optimization of the irrigation time and irrigation frequency by using Hydrus-2D and a capacitance FDR sensor

The evolution of water content on a sandy soil during the sprinkler irrigation campaign, in the summer of 2010, of a field of sugar beet crop located at Valladolid (Spain) is assessed by a capacitive FDR (Frequency Domain Reflectometry) EnviroScan. This field is one of the experimental sites of the Spanish research center for the sugar beet development (AIMCRA). The objective of the work focus on monitoring the soil water content evolution of consecutive irrigations during the second two weeks of July (from the 12th to the 28th). These measurements will be used to simulate water movement by means of Hydrus-2D. The water probe logged water content readings (m3/m3) at 10, 20, 40 and 60 cm depth every 30 minutes. The probe was placed between two rows in one of the typical 12 x 15 m sprinkler irrigation framework. Furthermore, a texture analysis at the soil profile was also conducted. The irrigation frequency in this farm was set by the own personal farmer 0 s criteria that aiming to minimizing electricity pumping costs, used to irrigate at night and during the weekend i.e. longer irrigation frequency than expected. However, the high evapotranspiration rates and the weekly sugar beet water consumption—up to 50mm/week—clearly determined the need for lower this frequency. Moreover, farmer used to irrigate for six or five hours whilst results from the EnviroScan probe showed the soil profile reaching saturation point after the first three hours. It must be noted that AIMCRA provides to his members with a SMS service regarding weekly sugar beet water requirement; from the use of different meteorological stations and evapotranspiration pans, farmers have an idea of the weekly irrigation needs. Nevertheless, it is the farmer 0 s decision to decide how to irrigate. Thus, in order to minimize water stress and pumping costs, a suitable irrigation time and irrigation frequency was modeled with Hydrus-2D. Results for the period above mentioned showed values of water content ranging from 35 and 30 (m3/m3) for the first 10 and 20cm profile depth (two hours after irrigation) to the minimum 14 and 13 (m3/m3) ( two hours before irrigation). For the 40 and 60 cm profile depth, water content moves steadily across the dates: The greater the root activity the greater the water content variation. According to the results in the EnviroScan probe and the modeling in Hydrus-2D, shorter frequencies and irrigation times are suggested.