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501.
502.
Dissolved Organic Matter in Forest Soils: Sources, Complexing Properties and Action On Herbaceous Plants 总被引:2,自引:0,他引:2
A. T. Kuiters 《Chemistry and Ecology》1993,8(3):171-184
Dissolved organic matter (DOM) is an important component of plant-soil systems. Its essential role in soil solution chemistry, soil-forming processes and its effects on biota, including soil fauna, bacteria, fungi and plants, is extensively documented in literature. in this contribution several forest leaf litter types are compared as sources of DOM and the released organics are subjected to gel permeation chromatography to reveal their molecular-size distribution. Moreover, complexing properties, as an indication for the podzolization potential of the litter leachates, were established. the occurrence and properties of DOM in different soil horizons were monitored beneath a stand of Scots pine. the effects of the different groups of soluble organics including phenolic, fulvic and humic acids, and of water-extractable humic substances on the performance of herbaceous plants of the forest floor are briefly reviewed. 相似文献
503.
SANJIB Kumar Das DIBYENDU Biswas SUDIPTO Roy 《应用与环境生物学报》2007,13(5):662-667
The benthic macroinvertebrate communities of two lotic aquatic habitats,namely,the Churni River(C-R)and the Jalangi River(J-R)were compared in this study.One lotic aquatic system(C-R)was polluted by organic pollutants due to discharge of unprocessed sewage water,while the other(J-R)was not affected by such pollution.Evaluations of various physico-chemical properties of water,sediment and different macroinvertebrate communities of the two tropical lotic systems were done in a period from January,2002 to December,2003.A long term temporal change in the macroinvertebrate communities was recorded due to increase in sediment rH value.Sediment redox potential affected by the anthropogenic activities was found to be an important factor for alteration of macroinvertebrate communities in these aquatic ecosystems.A positive correlation has been established between rH and Margalef index in this study.Potassium and the total count of coliform bacteria in water showed significantly higher values for the polluted Churni River than those for the Jalangi River.Fig 3,Tab 4,Ref 34 相似文献
504.
农药和其它有机化合物环境参数的相关性及其预测 总被引:5,自引:0,他引:5
农药和其它有机化合物的水溶解度、正辛醇/水分配系数、有机碳吸附常数和生物浓缩因子等物化参数之间存在着明显的相关性,有机化合物的水溶解度与其正辛醇/水分配系数、有机碳吸附常数和生物浓缩因子呈负相关;正辛醇/水分配系数与有机碳吸附常数和生物浓缩因子呈正相关。本文所建立的数学关系式能较好地预测未知化合物的环境特性。 相似文献
505.
通过对水稻盆栽试验,应用15N示踪测试技术和土壤农业化学分析方法,研究接种不同剂量固氮芽孢菌对当季水稻的供氮能力,结果表明:在施有机肥的基础上,接种固氮芽孢杆菌能为当季水稻提供氮素,而且,接菌剂量在0.60亿个?pot-1以内,其供氮能力随着接菌剂量的增加而提高;接种剂量从0.15亿个?pot-1增加到0.60亿个?pot-1,其对当季初的氮素供应从88.7mg?pot-1提高至109.7mg?pot-1,并减少水稻对肥料氮和土壤氮的吸收,增加茬后土壤的速效氮积累,接种量以0.15亿个?pot-1~0.30亿个?pot-1较经济。但在一定的施肥基础上,接种固氮菌对水稻的产生量和吸收氮素总量影响不明显。 相似文献
506.
Dynamics of soil organic matter in primary and secondary forest succession on sandy soils in The Netherlands: An application of the ROMUL model 总被引:2,自引:0,他引:2
M.A. Nadporozhskaya G.M.J. Mohren O.G. Chertov A.S. Komarov A.V. Mikhailov 《Ecological modelling》2006,190(3-4):399-418
We applied the simulation model ROMUL of soil organic matter dynamics in order to analyse and predict forest soil organic matter (SOM) changes following stand growth and also to identify gaps of data and modelling problems. SOM build-up was analysed (a) from bare sand to forest soil during a primary succession in Scots pine forest and (b) on mature forest soil under Douglas fir plantations as an example of secondary succession in The Netherlands. As some of the experimental data were unreliable we compiled a set of various scenarios with different soil moisture regime, initial SOM pools and amount and quality of above and below ground litter input. This allowed us to find the scenarios that reflect the SOM dynamics more realistically. In the Scots pine forest, total litter input was estimated as 0.50 kg m−2 year−1. Two scenarios were defined for the test runs: (a) forest floor moisture regimes—‘dry, mesic and hydric’ and (b) augmenting a root litter pool with three ratios of needles and branches to roots: 1:1, 1:1.5 and 1:2.0. The scenario finally compiled had the following characteristics: (a) climate for dry site with summer drought and high winter moisture of forest floor; (b) a litter input of 0.25 kg m−2 year−1 above ground and 0.50 kg m−2 year−1 below ground; (c) a low nitrogen and ash content in all litter fall fractions. The test runs for the estimation of the initial SOM pools and the amount and proportion of above and below ground litter fall were also performed in the Douglas fir plantation. The inputs of above ground litter tested in various combinations were 0.30 and 0.60 kg m−2 year−1, and below ground litter 0.30, 0.60 and 0.90 kg m−2 year−1. The scenario that fitted the experimental data had an SOM pool of 20–25 kg m−2, an aboveground litter input of 0.6 kg m−2 year−1and a below ground litter input of 0.9 kg m−2 year−1. The long-term simulation corresponded well with the observed patterns of soil organic matter accumulation associated with the forest soil development in primary and secondary succession. During primary succession in Scots pine forest on dry sand there is a consistent accumulation of a raw humus forest floor. The soil dynamics in the Douglas fir plantation also coincide with the observed patterns of SOM changes during the secondary succession, with SOM decreasing significantly under young forest, and SOM being restored in the older stands. 相似文献
507.
低分子量有机酸对可变电荷土壤吸附铝的影响机制 总被引:3,自引:0,他引:3
通过吸附性铝的解吸实验研究了低分子量有机酸对三种可变电荷土壤(2种砖红壤和1种赤红壤)吸附铝的影响机制,结果表明,柠檬酸、苹果酸和酒石酸等带有3个及3个以上活性官能团的有机酸在低pH条件下可以通过形成土壤一有机酸一铝三元表面络合物和增加土壤的表面负电荷两种机制显著增加土壤对铝离子的吸附量,但以前一种影响机制为主。乳酸、水杨酸、草酸和丙二酸等带有2个活性官能团的有机酸仅通过改变土壤的表面负电荷影响铝的吸附。土壤氧化铁是土壤吸附有机酸的主要载体,当用化学方法将土壤中的氧化铁除去后,有机酸对铝吸附的影响变小。在pH5.0时有机酸主要通过形成可溶性有机铝络合物减小土壤对铝的吸附,但有机酸的存在增加了Al^3 在吸附性铝中所占的比例,导致铝的解吸率增加。土壤中大量氧化铁的存在使其即使在低pH下也能对铝离子发生专性吸附,导致吸附性铝的解吸率减小。 相似文献
508.
天然水体中有机酸当量浓度的确定方法 总被引:3,自引:0,他引:3
本文根据天然水体中溶解有机在碳与化学需氧量和生化需氧量之间的相关性,以及有机酸当量和水体溶解有机碳之间的近似定量关系,提出了由化学需氧量或生化需氧量得到溶解有机碳或总有机碳浓度,最终得到有机酸和有机酸根当量浓度的转换方法,为大区域天然水体有机酸碱缓冲作用的评估提供了一个实用的转换途径。 相似文献
509.
不同有机物料在潮棕壤中有机碳分解进程 总被引:9,自引:2,他引:9
用尼龙网袋法研究了特定年度中,不同月份间有机物料在潮棕壤旱田、水田中有机碳分解速率及C/N变化。结果表明,4种物料(玉米秸和玉米根,水稻秸和水稻根)在潮棕壤地区温度、湿度适宜的前3个月(1999年7—月)迅速分解,之后进入缓慢分解阶段,其中根的分解残留率始终高于秸秆。经计算约有2/3的玉米根和稻根腐解产物残留在土壤里;分解至试验结束。所有物料的C/N比都趋于一致,约在10—13之间,与土壤腐殖质的洲比非常相近,说明这些物料已基本完成其腐殖化过程,而成为较稳定的有机组分、这对增加土壤有机质、培肥土壤非常重要。 相似文献
510.
概括了环境中可溶性有机物的特点,并系统总结了当前国内外关于可溶性有机物对土壤中主要污染物环境行为的影响的研究进展。阐述了可溶性有机物对农药、多环芳烃在土壤中的吸附、解吸及分配等环境行为所起的作用。最后指出了该方面研究存在的问题及今后应加强的方向。 相似文献