Multivariate modeling of acoustomechanical response of 14-year-old suppressed loblolly pine (<Emphasis Type="Italic">Pinus taeda</Emphasis>) to variation in wood chemistry,microfibril angle and density     

Charles?Essien  Brian?K.?ViaEmail author  Qingzheng?Cheng  Thomas?Gallagher  Timothy?McDonald  Xiping?Wang  Lori?G.?Eckhardt 《Wood Science and Technology》2017,51(3):475-492

The polymeric angle and concentration within the S₂ layer of the softwood fiber cell wall are very critical for molecular and microscopic properties that influence strength, stiffness and acoustic velocity of wood at the macroscopic level. The main objective of this study was to elucidate the effect of cellulose, hemicellulose, lignin, microfibril angle and density on acoustic velocity and material mechanical properties of 14-year-old suppressed loblolly pine. Cellulose, hemicellulose and density are consistently the most important drivers of strength, stiffness and velocity. Cellulose and lignin are the highest and lowest contributor to velocity, respectively, with lignin acting as a sound wave dispersant, while cellulose is the most important conductor of sound wave at the molecular level, while hemicellulose acts as a special coupling agent between these components. The polymeric constituents are thus important drivers of sound wave propagation at the molecular level, while density played a subsequent role at the macroscale.  相似文献   

Management effects on forms of phosphorus in soil and leaching losses   总被引：12，自引：0，他引：12  

P. Leinweber  R. Meissner  K. -U. Eckhardt  & J. Seeger 《European Journal of Soil Science》1999,50(3):413-424

We should know the effects of soil use and management on the contents and forms of soil phosphorus (P) and the resulting potential for leaching losses of P to prevent eutrophication of surface water. We determined P test values, amounts of sequentially extracted forms of P, P sorption capacities and degrees of P saturation in 20 differently treated soils and compared these data with leaching losses in lysimeters. One-way analyses of variance indicated that most fractions of P were significantly influenced by soil texture, land use (grassland, arable or fallow or reafforestation), mineral fertilization and intensity of soil management. Generally, sandy soils under grass and given large amounts of P fertilizer contained the most labile P and showed the largest P test values. Fallow and reafforestation led to smallest labile P fractions and relative increases of P extractable by H₂SO₄ and residual P. Arable soils with organic and mineral P fertilization given to crop rotations had the largest amounts of total P, labile P fractions and P test values. The mean annual concentrations of P in the lysimeter leachates varied from 0 to 0.81 mg l^–1 (mean 0.16 mg l^–1) and the corresponding leaching losses of P from < 0.01 to 3.2 kg ha^–1 year^–1 (mean 0.3 kg P ha^–1 year^–1). These two sets of data were correlated and a significant exponential function (R² = 0.676) described this relation. Different soil textures, land uses and management practices resulted in similar values for P leaching losses as those for the amounts of labile P fractions. Surprisingly, larger rates of mineral P fertilizer did not necessarily result in greater leaching losses. The contents of P extracted by NaHCO₃ and acid oxalate and the degrees of P saturation were positively correlated with the concentrations of P in leachates and leaching losses. As the P sorption capacity and degree of P saturation predicted leaching losses of P better than did routinely determined soil P tests, they possibly can be developed as novel P tests that meet the requirements of plant nutrition and of water protection.  相似文献   

Quebrada jaguay: early south american maritime adaptations     

DH Sandweiss  H McInnis  RL Burger  A Cano  B Ojeda  R Paredes  MC Sandweiss  MD Glascock 《Science (New York, N.Y.)》1998,281(5384):1830-1832

Excavations at Quebrada Jaguay 280 (QJ-280) (16 degrees30'S) in south coastal Peru demonstrated that Paleoindian-age people of the Terminal Pleistocene (about 11,100 to 10,000 carbon-14 years before the present or about 13,000 to 11,000 calibrated years before the present) in South America relied on marine resources while resident on the coast, which extends the South American record of maritime exploitation by a millennium. This site supports recent evidence that Paleoindian-age people had diverse subsistence systems. The presence of obsidian at QJ-280 shows that the inhabitants had contact with the adjacent Andean highlands during the Terminal Pleistocene.  相似文献