A new stylolite classification scheme to estimate compaction and local permeability variations

We modeled the geometrical roughening of bedding-parallel, mainly layer-dominated stylolites in order to understand their structural evolution, to present an advanced classification of stylolite shapes and to relate this classification to chemical compaction and permeability variations at stylolites. Stylolites are rough dissolution seams that develop in sedimentary basins during chemical compaction. In the Zechstein 2 carbonate units, an important lean gas reservoir in the southern Permian Zechstein basin in Germany, stylolites influence local fluid flow, mineral replacement reactions and hence the permeability of the reservoir. Our simulations demonstrate that layer-dominated stylolites can grow in three distinct stages: an initial slow nucleation phase, a fast layer-pinning phase and a final freezing phase if the layer is completely dissolved during growth. Dissolution of the pinning layer and thus destruction of the stylolite's compaction tracking capabilities is a function of the background noise in the rock and the dissolution rate of the layer itself. Low background noise needs a slower dissolving layer for pinning to be successful but produces flatter teeth than higher background noise. We present an advanced classification based on our simulations and separate stylolites into four classes: (1) rectangular layer type, (2) seismogram pinning type, (3) suture/sharp peak type and (4) simple wave-like type. Rectangular layer type stylolites are the most appropriate for chemical compaction estimates because they grow linearly and record most of the actual compaction (up to 40 mm in the Zechstein example). Seismogram pinning type stylolites also provide good tracking capabilities, with the largest teeth tracking most of the compaction. Suture/sharp peak type stylolites grow in a non-linear fashion and thus do not record most of the actual compaction. However, when a non-linear growth law is used, the compaction estimates are similar to those making use of the rectangular layer type stylolites. Simple wave-like stylolites are not useful for compaction estimates, since their growth is highly non-linear with a very low growth exponent. In the case where sealing material is collected at the tooth during dissolution, stylolites can act as barriers for local fluid flow as they intensify sealing capabilities of pinning layers. However, the development of teeth and spikes offsets and thus destroys continuous stylolite seams so that the permeability across the stylolite becomes very heterogeneous and they are no continuous barriers. This behavior is best shown in rectangular layer and seismogram pinning type stylolites that develop efficient fluid barriers at teeth tips but destroy sealing capabilities of layers by offsetting them at the flank, leading to a permeability anisotropy along 2-D stylolite planes. Suture/sharp peak stylolites can create fluid barriers if they collect enough sealing material. However, if the collecting material does not seal or if spikes offset the sealing material the stylolite leaks. We propose that our classification can be used to realistically estimate chemical compaction in reservoirs and gives an indication on how heterogeneous the permeability of stylolites can be

A new stylolite classification scheme to estimate compaction and local permeability variations

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Temperatura base para aparecimento de folhas e filocrono da variedade de milho BRS Missões Base temperature for leaf appearance and phyllochron of the BRS Missões maize variety

O objetivo deste trabalho foi estimar a temperatura base para aparecimento de folhas e o filocrono em uma variedade de milho em várias datas de semeadura e dois anos de cultivo. Um experimento de campo foi realizado em Santa Maria, Rio Grande do Sul (RS), com sete datas de semeadura. Foi utilizada a variedade BRS Missões em dois anos agrícolas consecutivos (2005-06 e 2006-07). O delineamento experimental foi blocos ao acaso com seis repetições. A parcela foi composta por três linhas de 5m de comprimento no espaçamento 0,8m x 0,21m. Em cada parcela, foram marcadas ao acaso três plantas na linha central nas quais foi realizada semanalmente a contagem do número de folhas completamente expandidas (NFE) e o total (NFT). A temperatura base variou entre épocas de semeadura de 4,5 a 12&deg;C, com média próxima de 8&deg;C, valor que foi usado no cálculo da soma térmica. O filocrono foi maior quando calculado com base no NFE do que com base no NFT e variou com a data de semeadura, de 50,0 a 69,9&deg;C dia folha-1 e de 39,6 a 59,8&deg;C dia folha-1, respectivamente, sendo o fotoperíodo uma possível causa da variação do filocrono entre épocas.<br>The objective of this study was to estimate the base temperature for leaf appearance and the phyllochron of a maize variety in several sowing dates and two growing seasons. A field experiment was conducted in Santa Maria, RS, with seven sowing dates using the BRS Missões variety in two growing seasons (2005-06 and 2006-07). The experimental design was a completely randomized blocks, with six replications. Plots were three 5 m rows in a 0.8m x 0.21m spacing. Three plants in the central row of each plot were randomly tagged, and the number of fully expanded leaves (NFE) and the number of leaf tips (NFT) were counted once a week on the tagged plants. The base temperature varied with sowing date from 4.5 to 12&deg;C and an average of about 8&deg;C was used to calculate thermal time. Phyllochron was higher when calculated on an NFE basis than on a NFT basis, and varied with sowing date from 50.0 to 69.9&deg;C day leaf-1 and from 39.6 to 59.8&deg;C day leaf-1, respectively, with photoperiod being a likely cause to explain the variation in the phyllochron with sowing date