Modelling the growth of young individuals of Pinus nigra on thin carbonate soils under climate change in Hungary

Climate change highly impacts on tree growth and also threatens the forest of the karstic terrains. From the 1980s the frequency of decay events of the Pinus nigra Arnold forests showed a marked increase in Hungary. To understanding the vulnerability of Pinus nigra forests to climate change on shallow karstic soils in continental-sub Mediterranean climatic conditions we developed the study of three sampled population in the typical karstic landscape of Veszprém in North Transdanubia. We built our model on non-invasive approach using the annual growth of the individuals. MPI Echam5 climate model and as aridity index the Thornthwaite Agrometeorological Index were used. Our results indicate that soil thickness up to 11 cm has a major influence on the main growth intensity, however, aridity determines the annual growth rate. Our model results showed that the increasing decay frequency in the last decades was a parallel change to the decreasing growth rate of pines. The climate model predicts the similar, increased decay frequency to the presents. Our results can be valid for a wider areas of the periphery of Mediterranean climate zone while the annual-growth based model is a cost-effective and simple method to study the vitality of pine trees in a given area.

Rainfall infiltration and soil hydrological characteristics below ancient forest, planted forest and grassland in a temperate northern climate

How rainfall infiltration rate and soil hydrological characteristics develop over time under forests of different ages in temperate regions is poorly understood. In this study, infiltration rate and soil hydrological characteristics were investigated under forests of different ages and under grassland. Soil hydraulic characteristics were measured at different scales under a 250-year-old grazed grassland (GL), 6-year-old (6yr) and 48-year-old (48yr) Scots pine (Pinus sylvestris) plantations, remnant 300-year-old individual Scots pine (OT) and a 4000-year-old Caledonian Forest (AF). In situ field-saturated hydraulic conductivity (Kfs) was measured, and visible root:soil area was estimated from soil pits. Macroporosity, pore structure and macropore connectivity were estimated from X-ray tomography of soil cores, and from water-release characteristics. At all scales, the median values for Kfs, root fraction, macroporosity and connectivity values tended to AF>OT>48yr>GL>6yr, indicating that infiltration rates and water storage increased with forest age. The remnant Caledonian Forest had a huge range of Kfs (12 to >4922mmh-1), with maximum Kfs values 7 to 15 times larger than those of 48-year-old Scots pine plantation, suggesting that undisturbed old forests, with high rainfall and minimal evapotranspiration in winter, may act as important areas for water storage and sinks for storm rainfall to infiltrate and transport to deeper soil layers via preferential flow. The importance of the development of soil hydrological characteristics under different aged forests is discussed.

Nuevas perspectivas sobre la histopatología de la infección de Pinus Radiata por Fusarium Circinatum

223 p.

Unidades de manejo para pinus: desenvolvimento e aplicação de metodologia em áreas de produção no oeste catarinense.

O presente trabalho teve por objetivos desenvolver e aplicar, no oeste catarinense, uma metodologia de estabelecimento de unidades de manejo para pinus a partir do mapeamento semi-detalhado de solos das áreas de estudo. Duas hipóteses de trabalho foram modeladas, ambas utilizando o sistema de produção de pinus local, que não faz correção da deficiência de nutrientes (ΔN): uma interpretação baseada na ausência de resposta ao melhoramento do ΔN, ou seja, que os tetos de produtividade independem dessa ação, sendo esse o modelo atual; e uma segunda interpretação considerando que a ausência do melhoramento do ΔN interfere nos tetos de produtividade do cultivo de pinus para as terras estudadas, modelo que representa um novo paradigma a ser testado. Cada polígono do mapa de solos detalhado foi associado a uma base de dados, que permitiu a definição dos graus de limitação das terras (ΔN, deficiência de água, deficiência de oxigênio, suscetibilidade à erosão e impedimentos ao manejo) para o cultivo do pinus. Conjuntos de critérios, considerando os diferentes graus de limitação alcançados para cada faixa de terra (polígonos do mapeamento de solos), definiram os guias para as classes de unidades de manejo para o cultivo de pinus. O mapeamento de solos semi-detalhado das áreas de produção identificou áreas mapeáveis associadas às classes de solos, em nível de ordem, Latossolos, Nitossolos, Cambissolos, Neossolos e Gleissolos. Essas cinco ordens geraram 36 unidades de mapeamento de solos. As limitações associadas aos atributos profundidade efetiva, relevo e presença de pedregosidade/rochosidade fizeram dos impedimentos ao manejo os fatores de limitação mais importantes para o cultivo de pinus das áreas mapeadas. Os quantitativos das classes de unidades de manejo para pinus dependeram de se considerar ou não a hipótese de resposta ao melhoramento do ΔN no sistema de manejo em uso na região. Na hipótese da ausência de resposta ao melhoramento do ΔN para a produção de pinus, temos os seguintes quantitativos: Apta superior com 113,14 ha (ou 7,5% da área mapeada); Apta inferior com 644,73 (ou 42,8% da área mapeada); Marginal superior com 408,35 (ou 27,1% da área mapeada); Marginal inferior com 277,58 ha (ou 18,4% da área mapeada) e Inapta com 63,2 ha (ou 4,2% da área mapeada). Ao se considerar a hipótese de uma resposta positiva ao melhoramento de ΔN para a produção de pinus e que o atual sistema de manejo não faz esse melhoramento, ocorre uma piora dos resultados, com muitas terras migrando das classes de unidades de manejo Apta (superior e inferior) para a classe Marginal superior.

The influence of organic amendments on soil aggregate stability from semiarid sites

Restoring the native vegetation is the most effective way to regenerate soil health. Under these conditions, vegetation cover in areas having degraded soils may be better sustained if the soil is amended with an external source of organic matter. The addition of organic materials to soils also increases infiltration rates and reduces erosion rates; these factors contribute to an available water increment and a successful and sustainable land management. The goal of this study was to analyze the effect of various organic amendments on the aggregate stability of soils in afforested plots. An experimental paired-plot layout was established in southern of Spain (homogeneous slope gradient: 7.5%; aspect: N170). Five amendments were applied in an experimental set of plots: straw mulching; mulch with chipped branches of Aleppo Pine (Pinus halepensis L.); TerraCotten hydroabsobent polymers; sewage sludge; sheep manure and control. Plots were afforested following the same spatial pattern, and amendments were mixed with the soil at the rate 10 Mg ha-1. The vegetation was planted in a grid pattern with 0.5 m between plants in each plot. During the afforestation process the soil was tilled to 25 cm depth from the surface. Soil from the afforested plots was sampled in: i) 6 months post-afforestation; ii) 12 months post-afforestation; iii) 18 months post-afforestation; and iv) 24 months post-afforestation. The sampling strategy for each plot involved collection of 4 disturbed soil samples taken from the surface (0–10 cm depth). The stability of aggregates was measured by wet-sieving. Regarding to soil aggregate stability, the percentage of stable aggregates has increased slightly in all the treatments in relation to control. Specifically, the differences were recorded in the fraction of macroaggregates (≥ 0.250 mm). The largest increases have been associated with straw mulch, pinus mulch and sludge. Similar results have been registered for the soil organic carbon content. Independent of the soil management, after six months, no significant differences in microaggregates were found regarding to the control plots. These results showed an increase in the stability of the macroaggregates when soil is amended with sludge, pinus mulch and straw much. This fact has been due to an increase in the number cementing agents due to: (i) the application of pinus, straw and sludge had resulted in the release of carbohydrates to the soil; and thus (ii) it has favored the development of a protective vegetation cover, which has increased the number of roots in the soil and the organic contribution to it.

Raman spectroscopy of some complex arsenate minerals—implications for soil remediation

The application of spectroscopy to the study of contaminants in soils is important. Among the many contaminants is arsenic, which is highly labile and may leach to non-contaminated areas. Minerals of arsenate may form depending upon the availability of specific cations for example calcium and iron. Such minerals include carminite, pharmacosiderite and talmessite. Each of these arsenate minerals can be identified by its characteristic Raman spectrum enabling identification.