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Weathering of a calcalkaline granite was studied in the south of Galicia (NW Spain) where the average annual precipitation is 1400 mm and the average annual temperature is 12°C. The original rock contains perthitic K-feldspars, plagioclases with inclusions of muscovite and opaque minerals, quartz and chloritized biotite, with apatite, zircon, sphene and opaques as accessories. In the saprolite the structure of the rock is preserved, the plagioclases show up to grade 4 weathering and the biotites, between 2 and 3. Weathering in quartz and potassium feldspar crystals is manifested only by fracturing. Biotite changes following the parallel linear model and its weathering products are interstratified biotite–vermiculite and iron oxyhydroxides. The plagioclases change to a microgranular material by pseudomorphic transformation. This material, which substitutes the plagioclase, includes small clearly delimited units which retain zones with the optic characteristics of muscovite. X-ray diffraction analyses of microsamples show that they are formed by 1:1 diocthaedral phyllosilicate, smectite and a small quantity of mica. From these facts we concluded that smectite is formed inside the plagioclase crystals, and probably originates from the inclusions of muscovite contained in these crystals, as it is suggested by the microscopic study which shows the increase in volume which occurs when the crystals of muscovite are transformed. 相似文献
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As a consequence of global warming, additional areas will become ice-free and subject to weathering and soil formation. The most evident soil changes in the Alps will occur in proglacial areas where young soils will continuously develop due to glacier retreat. Little is known about the initial stages of weathering and soil formation, i.e. during the first decades of soil genesis. In this study, we investigated clay minerals formation during a time span 0-150 years in the proglacial area of Morteratsch (Swiss Alps). The soils developed on granitic till and were Lithic Leptosols.Mineralogical measurements of the clay (< 2 μm) and fine silt fraction (2-32 μm) were carried out using XRD (X-ray Diffraction) and DRIFT (Diffuse Reflectance Infrared Fourier Transform). Fast formation and transformation mechanisms were measured in the clay fraction. The decreasing proportion of trioctahedral phases with time confirmed active chemical weathering. Since the start of soil formation, smectite was actively formed. Some smectite (low charge) and vermiculite (high charge) was however already present in the parent material. Main source of smectite formation was biotite, hornblende and probably plagioclase. Furthermore, irregularly and regularly interstratified clay minerals (mica-HIV or mica-vermiculite) were formed immediately after the start of moraine exposure to weathering. In addition, hydroxy-interlayered smectite (HIS) as a transitory weathering product from mica to smectite was detected. Furthermore, since the start of soil evolution, kaolinite was progressively formed. In the silt fraction, only little changes could be detected; i.e. some formation of an interstratified mica-HIV or mica-vermiculite phase.The detected clay mineral formation and transformation mechanisms within this short time span confirmed the high reactivity of freshly exposed sediments, even in a cryic environment. 相似文献
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皖南网纹红土的剖面风化特征及其古气候意义 总被引：4，自引：0，他引：4
气候变化下土壤物质过程的响应特征是全球变化研究的重要主题。选取安徽宣城剖面,通过元素分析,对其风化强度特征进行了研究。结合与黄土高原第四纪黄土、古土壤、江苏镇江下蜀土以及江西九江红土等典型风成堆积剖面的对比分析,得出以下结论:(1)宣城红土剖面经历了高强度的化学风化作用,长石损失殆尽,进一步的风化作用已导致其含K矿物(黑云母、伊利石和钾长石)的分解,次生粘土矿物以高岭石为主。此外,宣城红土与其他剖面相比,显著强于镇江下蜀土,远强于洛川黄土与古土壤,而与九江红土的风化程度较为相近。(2)在地形、母岩等条件相似的情况下,气候(特别是温度和降水量)是控制化学风化程度的主要因素,并且与温度相比降水因素可能起着更为重要的制约作用。(3)在地质历史时期,宣城→镇江→洛川,随着地域的北移,气候环境向干冷方向发展。(4)BA,Na/K和硅铁铝率的剖面变化特征揭示,中更新世早、中期,气候相对温暖潮湿,之后气候总体恶化,向干冷方向发展。但在此过程中,伴随着大姑-庐山间冰期和末次间冰期的到来气候又出现过两次短暂的回暖过程,并且在晚更新世早期呈现兼有干湿交替的特征。 相似文献
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Geanina Bireescu;Carmelo Dazzi;Giuseppe Lo Papa 《国际水土保持研究(英文)》2018,6(4):325-330
Soil morphological, physical and chemical properties are described at four locations along an elevational transect in the northeastern part of the Moldavian Plateau (Romania). These data contribute to the knowledge of the soils of this area and to their classification according to the USDA-Soil Taxonomy, FAO-WRB and the SRTS-Romanian System. The soils were classified as Inceptisols, Alfisols and Mollisols, according to the USDA-Soil Taxonomy; Gleysol, Chernozem and Luvisol, according to the FAO-WRB and Gleiosol, Cernoziom, Preluvosol, Luvosol, according to the SRTS-Romanian System. The selected soils have a range of properties that represent the soilscape of the Moldavian subcarpathian plateau, characterised by a natural forest with oak as the dominant species. The selected soil parameters decreased with increasing elevation; calcium carbonate and clay leaching and accumulation are the main soil formation processes.View The PDF 相似文献
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To examine the rate of chemical weathering, field experiments using microweight-loss techniques were carried out. Two kinds of porous rhyolite forming lava domes in Kozu-shima Island were selected: (1) a younger rock (weathering period is 2.6 ka) and (2) an older rock (20 ka). Both rocks seem to have been very similar in their initial composition and structure. They have, however, different properties in the present depending on the difference in weathering period. Rock tablets of these rhyolites with a diameter of 3.5 cm and a thickness of about 1 cm were enclosed in a nylon mesh bag and placed in a soil–bedrock interface on a hillslope of central Japan for over 5 years. The younger rock has a lower weight loss by about 0.5%, and the older rock has a higher weight loss of 3% to 5%. These results show that older rock has a higher rate of chemical weathering than in younger rock. This supports Oguchi et al.'s (Oguchi, T.C., Hatta, T., Matsukura, Y., 1994. Changes in rock properties of porous rhyolite through 40,000 years in Kozu-shima Island, Japan. Geogr. Rev. Jpn. 67A, 775–793 (in Japanese, with English Abstr.); Oguchi, T.C., Hatta, T., Matsukura, Y., 1999. Weathering rates over 40,000 years based on changes in rock properties of porous rhyolite. Phys. Chem. Earth (A) 24, 861–870.) finding that the rate of change in chemical properties appears to accelerate with weathering time. 相似文献
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In alpine environments, climate change may alter vegetation composition as well as the quantity and quality of plant litter, which in turn may affect microbial community composition and functioning. In this study, we analyzed soil microbial community composition and its activity along a vegetation gradient (900-1900 m above sea level (a.s.l.)) in the Austrian Limestone Alps. Soil pH and C:N ratios were significantly different under different plant communities and ranged from 3.9 to 6.1 and from 29 to 17, respectively. The highest amounts of microbial biomass, estimated by the sum of microbial phospholipid fatty acids (total PLFAs), were found at sites with high pH and low C:N ratio, i.e. in alpine grassland and beech forest sites (3.9 ± 0.05 and 3.4 ± 0.7 μmol per g organic carbon (OC), respectively), and the lowest amounts were found at sites with low pH and high C:N ratio, i.e. sites with high percentage of conifers and acidophilic vegetation (around 2 μmol (g OC)−1). Total and bacterial PLFAs as well as microbial activity (dimethyl sulphoxide reduction) did not show consistent altitudinal trends. The fungal PLFA 18:2ω6,9 was significantly higher in the forest sites (between 9.2 and 6.7 mol%) compared to the shrubland and grassland sites (between 4.5 and 2.3 mol%). A similar trend was found for ergosterol contents. As a consequence, the bacterial to fungal biomass ratio increased significantly from forest sites to shrubland and grassland sites. Expected future upward migration of the tree line in alpine environments in response to climate warming will therefore increase the abundance of fungi in these ecosystems. 相似文献
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Denis L. Guerra Helen C.P. Oliveira Paulo C. Corrêa da Costa Rúbia R. Viana Claudio Airoldi 《CATENA》2010
The original smectite clay mineral has been collected from Amazon region, Brazil. The compound 2-aminomethylpyridine (AMP) was anchored onto Amazon smectite surface by heterogeneous route. The natural (SMC) and modified (SMCAMP) smectite samples were characterized by elemental analysis, scanning electron microscopy, N2 adsorption, X-ray diffraction, and silicon-29 and carbon-13 nuclear magnetic resonance. Due to the increment of basic centers attached to the pendant chains, the metal adsorption capability of the final chelating material, was found to be higher than the precursor. The ability of these materials to remove Cr(VI) from aqueous solution was followed by a series of adsorption isotherms at room temperature and pH 4.0. The maximum number of moles adsorbed was determined to be 1.16 and 1.87 mmol g− 1 for SMC and SMCAMP, respectively. In order to evaluate the clay samples as adsorbents in dynamic system, a glass column was fulfilled with clay samples (1.0 g) and it was fed with 2.0 × 10− 4 mol dm− 3 Cr(VI) at pH 4.0. The energetic effects caused by metal cation adsorption were determined through calorimetric titrations. Thermodynamics indicated the existence of favorable conditions for such Cr(VI)–nitrogen interactions. 相似文献
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研究地形对黑土区坡面侵蚀-沉积空间分布特征的影响可以为水土保持措施配置提供科学依据。以典型黑土区——黑龙江省宾县东山沟小流域为研究区域,在流域上游、中游和下游各选取2个典型坡面,坡面种植作物均为玉米。典型坡面坡顶、坡上、坡中、坡下和坡脚的平均坡度分别为3.1°,3.0°,4.0°,2.8°,1.2°。利用137Cs示踪技术,分析了坡度、坡长和坡形对坡面侵蚀—沉积空间分布特征的影响。结果表明:研究流域农耕地坡面以侵蚀为主,平均侵蚀速率为448 t km~(~(-2)) a~(~(-1)) ;坡面不同部位土壤侵蚀—沉积分布特征差异明显,坡顶、坡上、坡中和坡下主要表现为侵蚀,平均侵蚀速率分别为819、376、1 000和634 t km~(~(-2)) a~(~(-1)) ,而坡脚表现为明显的沉积,平均沉积速率为~(~(-1)) 382 t km~(~(-2)) a~(~(-1)) 。不同坡形坡面侵蚀-沉积分布存在差异,凸形坡坡面表现为先侵蚀后沉积的分布特征,而复合坡坡面呈现出侵蚀-沉积交错分布特征;坡面土壤侵蚀速率与坡度和坡长均呈极显著的幂函数关系,而坡度对黑土区坡面侵蚀的影响明显大于坡长,反映了即使在长坡缓地形的黑土区坡度对侵蚀的影响仍然有重要作用。因此,在黑土区配置合理的水土保持措施时,应尽量削弱坡度对坡耕地土壤侵蚀的影响。 相似文献
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南极半岛海洋气候区的土壤I.风化作用 总被引：2，自引：0，他引：2
南极海洋性气候区是南极风化与成土作用相对较强的地区。本在对本区气候特点进行分析的基础上,明确了冻胀风化是本区最主要的物理风化形式,强烈的现代地貌过程对本区风化与成土过程具有显影响。阐述了本区内化学风化的主要过程、机制与产物,同时指出生物因素在本区的岩石风化与原始土壤形成过程具有重要意义。 相似文献
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This study was undertaken to study the impact of adding <75 μm elemental sulfur (ES) on P availability from a range of <250 μm ground rock phosphates (RP) namely; Minjingu (Mi) from Tanzania, Khouribga from Morocco (Mo) and Duchess (D) from Australia. Italian ryegrass (Lolium multiflorum, Thumpa tetraploid) grown in a glasshouse was used as the test crop and tops were harvested 5 times over 27 weeks. Co-granulating RP and 10.7% ES yielded 30–70% more ryegrass tops than RP alone, with the greatest effect with Mi. Fertilizer P recovery in the tops from the RP was 5.2% with D and 6.5% and 7.8% from Mi and Mo, respectively. ES addition increased this by 51% from Mo, 98% from D and 194% from Mi. Co-granulation of RP with ES has been shown to be an effective means of releasing plant available P to crops from RP with minimal fertilizer processing. 相似文献
13.
Sheng Zhang;Ji Liu;Ying Feng;Xingming Hao;Yanning Liang;Lihua Xue;Xiaoning Zhao; 《European Journal of Soil Science》2024,75(2):e13474
With the rapid expansion of agriculture on saline–alkaline soils, environmental problems such as increased greenhouse gas (GHG) emissions, eutrophication and soil degradation are becoming increasingly serious. To clarify the characteristics of carbon (C) and nitrogen (N) cycling and their loss mechanisms in cultivated saline–alkaline soils, an undisturbed soil column experiment was conducted to analyse C and N leaching and GHG emissions by applying different fertilizer rates. The experiment had six treatments using N-(NH4)SO4 over a 40-day seedling stage, with and without maize. Treatments were: no N with maize (0Nmaize: 0 kg N ha−1), reduced N with maize (RNmaize: 63 kg N ha−1), conventional N with maize (CNmaize: 160 kg N ha−1) and their equivalents without maize (0Nsoil: 0 kg N ha−1; RNsoil: 63 kg N ha−1; CNsoil: 160 kg N ha−1). The results indicated that reduced N with maize reduced the N2O emission by 21%, with N leaching (TN: 41%, NO3−–N: 19%, NH4+ − N: 63%) within 15 days after fertilization, but had no significant effect on CH4 emission compared to conventional N with maize. Therefore, reduced N with maize had the smallest N loss, which accounted for 1.5% of the relative percentage of N flow including N2O (0.3%), N leaching (2%), aboveground biomass N (76%) and root biomass N (22%). Compared to conventional N with maize, reduced N with maize significantly reduced N leaching by 40% because conventional N with maize greatly exceeded the crop N uptake when maize root length was only within 20 cm. Reduced N without maize reduced CO2 emission (19%) compared to conventional N without maize. Uncultivated saline–alkaline soils face greater N overuse and leaching risk because higher NO3−–N leaching (6.9 mg L−1) that occurred in bare soils without fertilization, which increased by 2.6–3.6 times when the N input increased from 63 to 160 kg N ha−1 compared to control. In conclusion, reducing conventional N fertilizer inputs by 60% is not only an effective strategy to reduce CO2 and N2O emission and N leaching but also effectively absorbs C, and the N retained in the soil tillage layer can help to meet maize seedling growth requirements in Solonchaks. 相似文献
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Profile development indices of Harden [Harden, J.W., 1982. A quantitative index of soil development from field: examples from a chronosequence in Central California. Geoderma 285, 1–98] and Ferrari and Magaldi [Ferrari, G., Magaldi, D., 1983. Significato ed applicazioni della paleopedologia nella stratigrafia del Quaternario. Boll. Mus. Civ. St. Nat. Verona 10, 315–340] have shown their utility for comparative dating of some paleosols during geomorphological and geological surveys. In Italy and other countries, pedostratigraphic methods have been commonly applied to soil profiles formed in continental formations. Unfortunately, buried and relict paleosols are very scarce or badly preserved in some areas of Italy due to past and recent tectonic activity and to strong human impact dating back to prehistoric times.In order to use relict paleosols for correct chronostratigraphic interpretation of relict paleosols and in order to correlate them with old landscape forms for the reconstruction of Quaternary sequences, a new micromorphological index (MISODI) for assessing soil development and degree of weathering was devised. The index was tested in the extensional tectonic basin of L'Aquila-Scoppito (Abruzzi, Central Italy) where some chronostratigraphic information is available.Results demonstrate that there is a good relationship between presumed relative age of paleosols and degree of weathering and pedogenesis in B and B/C horizons as assessed by this index. The index has the potential to be adapted for application to other paleosol types in other countries. 相似文献
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硫杆菌和元素硫在治理重金属污染中的应用研究进展 总被引：1，自引：0，他引：1
硫杆菌和元素硫在治理土壤和沉积物中重金属已经有了较多的研究。本文论述了利用硫杆菌和元素硫治理土壤和沉积物中的重金属污染的应用进展。主要包括了利用硫杆菌和元素硫去除重金属的优缺点及主要的影响因素,如温度、pH、细菌种类、元素硫浓度等。 相似文献
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城市地貌决定着城市的布局和发展方向等方面。以咸阳市为例,对DEM数据进行分析,利用ArcGIS软件分析高程、坡度、坡向3个地貌要素。经过分析得出,咸阳市地貌类型包括河漫滩、一级阶地、二级阶地、三级阶地和黄土台塬,从渭河向两侧地势呈阶梯状抬升;咸阳市区绝大部分为平坡地(0°～5°),占总面积的83.6%;其次是缓坡地(5°～15°),占总面积的11.8%;其余坡地所占比例甚少。咸阳市区西南、南、东南3面坡向占总面积的60.8%,其中以东南坡向为主,占34.6%;而西北、北、东北3面坡向占总面积的18.9%。咸阳市沿着渭河东西发展,道路交通以及排水系统受阶梯地形影响很大。 相似文献
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滇中地区4种覆被类型地表径流的氮磷流失特征 总被引：3，自引：1，他引：3
采用径流小区研究自然降雨条件下,滇中地区4种覆被类型(荒坡灌草丛、云南松林、针阔混交林、桉树人工林)2010年雨季的径流量、泥沙输出量、氮磷流失量及动态变化特征。结果表明:年累积地表径流量和泥沙输出量荒坡灌草丛(7.14m~3/hm~2,0.06kg/hm~2)显著低于其它3种覆被类型,针阔混交林(29.38m~3/hm~2,0.31kg/hm~2)显著低于云南松林(46.26 m~3/hm~2,0.79kg/hm~2)和桉树人工林(49.18 m~3/hm~2,1.66kg/hm~2),云南松林和桉树人工林无显著差异;4种覆被类型降雨—径流呈对数关系,变率dy/dx大小顺序为荒坡灌草丛针阔混交林云南松林桉树人工林;荒坡灌草丛、针阔混交林、云南松林和桉树人工林溶解性TN流失量分别为5.24,15.96,26.61,46.5g/hm~2,颗粒态TN流失量分别为8.83,8.59,69.15,88.57g/hm~2,溶解性TP流失量分别为0.19,0.90,1.52,4.89g/hm~2,颗粒态TP流失量分别为0.44,2.31,4.73,12.04g/hm~2,各覆被类型之间均存在显著性差异,其中桉树人工林氮磷流失显著高于其它覆被类型,表明结构单一的人工林控制水土流失能力较差;4种覆被类型氮磷流失量与地表径流量、泥沙输出量均呈极显著正相关关系,且以泥沙结合态为主,因此控制泥沙输出是减少研究区面源污染负荷的重要措施。 相似文献
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Azhar Mehmood Asif Tanveer Muhammad Mansoor Javed Muhammad Ather Nadeem Muhammad Naeem 《Archives of Agronomy and Soil Science》2018,64(2):208-218
Alligator weed (Alternanthera philoxeroides) is the most troublesome invasive weed in transplanted rice ecosystems worldwide. A two-year field study was conducted to estimate economic threshold levels and the season long competitive effect of six alligator weed densities (0, 2, 4, 8, 16, and 32 plants m?2) on yield and quality traits of transplanted rice. A gradual linear incline in dry weight of alligator weed was observed with an increase in its density from 2 to 32 plants m?2. Maximum N (15.93–18.26 kg ha?1), P (15.10–16.46 kg ha?1) and K (16.34–17.81 kg ha?1) uptake by alligator weed was recorded at its density of 32 plants m?2. More micronutrient loss to the tune of 6.53, 47.92, 19.99, and 38.42 mg kg?1 for Cu, Fe, Zn, and Mn, respectively was observed at the same density. Increasing density of alligator weed caused more losses in paddy yield (up to 21.37–23.78%), amylose and rice grain protein contents. According to a nonlinear hyperbolic regression model, maximum paddy yield loss of rice at asymptotic value of alligator weed density was 38.8% during 2011 and 42.4% during 2012. Economic threshold value of alligator weed was estimated 1.5 and 1.3 plants per m2 during 2011 and 2012, respectively. 相似文献
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在3S技术支持下,采用景观面积比、分维数、多样性指数、斑块密度等景观格局指数及土地利用/覆盖综合动态变化度,分析了三峡库区巫溪县不同坡度带及坡向带的景观格局现状及变化。结果表明,不同景观类型在同一坡度带及坡向带的景观格局状况不同,同一景观类型在不同坡度带及坡向带亦不同。坡度与坡向对巫溪县景观格局状况及变化存在重要影响,且该影响陡坡比缓坡变化强烈,阴坡比阳坡变化强烈。 相似文献