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1.
Thirty soils differing widely in origin, texture and organic carbon content were used to study crust properties and development under laboratory conditions. Crust strength was measured as penetration resistance to an upward moving probe both with and without artificial rain treatment. The patterns of penetration resistance with time of drying under infra-red lamps varied considerably, the time taken to reach maximum and steady values for penetration resistance varying from 4 to 10 days. Maximum penetration resistance values ranged from approximately 50 to 500 kPa with one Iraqi soil recording a value of 800 kPa. The soils separated into 3 fairly distinct groups when penetration resistance was plotted against moisture content: Group I showed a sudden and sharp increase, Group II a gradual increase, whereas Group III did not show a definite relationship. A positive linear relationship was found between maximum penetration-resistance values of soils with and without artificial rain treatment. There was also a high positive correlation between small (2?0.53 mm) water-stable aggregates and penetration resistance and a negative correlation between penetration resistance and percentage water-stable aggregates of > 2 mm in size.In seedling emergence trials with spring barley (Hordeum vulgare L.), maximum emergence (90–98%) was recorded at penetration resistance (no rain treatment) of 75–110 kPa and zero emergence at approximately 300 kPa, with a good negative relationship between these values. There was a positive relationship between seedling emergence and penetration resistance values < 75 kPa, failure to emerge being due to a lack of anchorage and radial support for the shoot. Simulated rain treatment, which led to additional crust strength, reduced seedling emergence further for the limited number of soils tested. 相似文献
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Anna Kusumawati Benito Heru Purwanto Makruf Nurudin 《Soil Science and Plant Nutrition》2020,66(1):206-213
ABSTRACT Sugarcane is a strategic commodity in Indonesia. It is usually raised in a monoculture system. There is a lack of information about the effects of extended sugarcane monoculture on the soil carbon fraction. The aim of this study was to determine the relative changes in the soil organic C fractions in response to the duration of sugarcane monoculture on Entisols, Inceptisols, and Vertisols. The measured variables were the percentages of sand, silt, and clay, organic matter (OM), total nitrogen (TN), pH (H2O), cation exchange capacity (CEC), NH4 +, NO3 -, labile carbon fraction (soil carbon mineralization (C-Min), soil microbial carbon (C-Mic), and carbon particulate organic matter (C-POM)), and stable carbon fraction (humic and fulvic acids). Soil type with sugarcane monoculture period had significant influences on the percentages of clay, sand, silt, CEC, and pH (H2O). Soil type and sugarcane monoculture period had no apparent significant effect on C-Min or C-POM but did significantly influence C-Mic. The humic and fulvic acid levels in all three soil types were affected by the duration of sugarcane monoculture. To establish the impact of long-term sugarcane monoculture on the physicochemical properties of soils with various textures, it is more appropriate to measure the soil stable carbon fractions such as humic and fulvic acid rather than the soil labile carbon fractions such as C-Min, C-POM, or C-Mic. 相似文献
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Dr Marcin Pietrzykowski Wojciech Krzaklewski 《Archives of Agronomy and Soil Science》2013,59(5):473-483
Abstract The work presents study results on the formation of humus horizons, the accumulation of organic carbon and nitrogen as well as humus composition in successional and reclaimed soils in a sand mine cast in southern Poland. Research plots were designed in chronosequence: 5, 17, 20 and 25 years. Increased thickness of humus horizon and accumulation of organic carbon was reported both in successional soils and in reclaimed soils. However, in corresponding age groups of reclaimed soils these characteristics were two times as high as in successional soils. The estimated accumulation rate of organic carbon (Corg) was three times higher and total nitrogen (Nt) five times higher in reclaimed soils than in successional soils. In both types of soils there was an increase in the amount of carbon trapped with humic and fulvic acid (CHa + CFa) and structure of humic acids. Studies indicated that reclamation treatment significantly accelerated soil-formation in opencast sand mine. 相似文献
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THE ACCUMULATION OF SOIL ORGANIC MATTER AND ITS CARBON ISOTOPE CONTENT IN A CHRONOSEQUENCE OF SOILS DEVELOPED ON AEOLIAN SAND IN NEW ZEALAND 总被引：1，自引：0，他引：1
Soil organic matter was extracted by a mixture of O.IM Na4P2O: O.IM NaOH from a chronosequence of weakly weathered soils developed on aeolian sand, and fractionated into humin (non-extractable), humic acid, and fulvic acid. The mass of total organic carbon in the profiles, the 14C content and the 13C/12C ratios were also determined. The weight of total carbon increased rapidly at first and then gradually without attaining a steady state. This trend was also shown by the humin and fulvic acid fractions, but the humic acid fraction appeared to have reached a maximum after about 3000 years. The order of total weights of the organic fractions was humin > fulvic acid > humic acid. The evidence suggests that the proportions of the humic fractions formed by decomposition are related to soil differences but not to vegetation. The greater part of the plant material found in the soils appears in the humin and fulvic acid fractions. 相似文献
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Soil erosion by water causes substantial on‐site degradation and off‐site damages in the densely populated state of North Rhine‐Westphalia (Germany). Measures of soil conservation should be adjusted to soil erodibilities and should be based on an understanding of the processes involved in water erosion including aggregate breakdown, rainsplash erosion, surface sealing, and soil loss. For a state‐wide assessment of erosion processes and erodibilities, we tested representative cultivated soils of North Rhine‐Westphalia in laboratory and field experiments with artificial rain. In the laboratory experiments described in this paper, rainsplash erosion, sealing susceptibility, and interrill erodibility of 25 topsoils filled in 0.5 m2 boxes were investigated. Results of different aggregate‐stability tests correlate with organic‐matter contents but not with parameters of rainsplash or soil loss. On most soil materials, rainsplash increases or maintains constant rates in the course of the simulation runs indicating that the soil surface did not attain a higher shear resistance. High sealing susceptibilities are found for soils of quite different textures ranging from loam sand to silt clay, whereas other silt clays, clay loams, and some clay silts maintain high infiltration rates. A trend of increasing sealing susceptibility and total soil loss with increasing clay content is observed for the loam sands to sand loams. Dynamics of soil loss is largely governed by runoff rates. Total soil loss is also determined by sediment concentration in surface runoff, which is low on most clayey soils, on loam sands poor in clay, and on a sand loam, and high in the case of highly erodible clay silts, loam sands, and sand loams. The most crust prone soils are not necessarily the most erodible. On most soils, soil‐loss rates do not stabilize until the end of the rainfall experiments. For comparing the interrill erodibilities of the soils, total soil loss is preferred instead of interrill erodibility factors (Ki, Kiq) published in the literature. 相似文献
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白浆土是吉林省和黑龙江省东部地区的主要农田土壤之一,研究白浆土对腐殖酸的吸附作用,可为探究白浆土的固碳潜力提供理论依据。采用批量平衡法,分析不同有机碳含量的白浆土及其组分(包括去有机质土壤、粉粒、黏粒)对腐殖酸的吸附动力学和等温吸附特性。结果表明:随吸附时间的延长,白浆土及其各组分对腐殖酸的吸附量逐渐增加;整个吸附动力学过程可划分为快速(0～30 min)和慢速(30～480 min)反应阶段,伪二级动力学方程的拟合效果优于Elovich、双常数和伪一级动力学方程。白浆土及其各组分对腐殖酸的吸附量随腐殖酸初始浓度的增加逐渐增大,Langmuir方程的拟合效果通常优于Freundlich方程和Temkin方程。随白浆土有机碳含量的增加,其对腐殖酸的最大吸附量分别为26.9,24.1,15.6 mg/g。而白浆土不同组分相比,最大吸附量的顺序依次为黏粒>去有机质土壤>粉粒,黏粒对腐殖酸的吸附量分别是原土的2.15～3.88倍,去有机质土壤的1.61～2.21倍,粉粒土壤的7.90～8.65倍。有机碳含量低的白浆土对腐殖酸具有更强的吸附能力,黏粒含量高的白浆土对腐殖酸的吸附潜力更大。 相似文献
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Jude C. Obi 《Archives of Agronomy and Soil Science》2013,59(10):1473-1490
This study established the influence of particle size fractions (psf) on the characteristics of coastal plain soils of southeastern Nigeria. A total of 180 samples were collected according to genetic horizons on 30 profile pits prepared on the upper, middle, and lower slope positions of 10 toposequences. The samples were analyzed for hydraulic conductivity, pH, bulk density, moisture content, electrical conductivity, exchangeable bases and acidity, organic carbon, available and total phosphorus (P) contents, dithionite citrate bicarbonate (DCB) extractable and amorphous iron and aluminum (Al) contents. Particle size distribution was also analyzed, including total sand, very coarse, coarse, medium, fine and very fine sand, clay, and silt. Statistical analysis carried out included analysis of variance, correlation, and principal component. Very coarse sand influenced the distribution of P and DCB-Al within the toposequences. Active pedogenesis was located in the fourth horizons of the profiles that manifest inverse relationship of very coarse sand with P and amorphous Al. The association between sand particles and sesquioxides, especially of Al, was responsible for the low pH associated with coastal plain soils. Principal component analysis confirmed that total sand fractions are the determinants of rate and extent of pedogenesis and influences the properties of coastal plain soils. 相似文献
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《Soil biology & biochemistry》1990,22(1):35-41
To determine why viability of conidia of Cochliobolus sativus declines in some soils treated with atrazine and not in others, the influence of soil organic matter, texture and pH on the lethal effect of atrazine was examined. Viability of conidia on Boyer sandy loam (SL) (−1 kPa matric potential) containing 25μg atrazine g−1 was 7% after 3 weeks, as compared with 99% in the control. Decreasing the organic carbon of Boyer SL from 0.73 to 0.02% by H2O2 digestion, or to 0.04% by NaOH extraction, nullified the lethal effect of atrazine. The addition of 4mg humic acid g−1 to NaOH-extracted Boyer SL containing atrazine partially restored the lethal effect. Increasing the pH of Boyer SL from 5.2 to 7.5 nullified the lethal effect of atrazine. Viability of conidia on Spinks SL (pH 6.6) containing atrazine remained at 99% after 3 weeks. The addition of 4mg humic acid g−1 from Boyer SL to atrarine-treated Spinks SL reduced viability to 86%. Viability of conidia in atrazine-treated acidified Spinks SL (pH 5.4) was 65%. The response of conidia to atrazine in soils supplemented with 4% bentonite clay, or in separated sand or silt and clay fractions of soils was not affected except when the soil pH was altered. Thus, a low pH and the presence of humic acid increased the toxicity of atrazine to conidia of C. sativus. 相似文献
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To understand the dynamics of soil organic matter in humid regions in Asia, several soil and meteorological properties were tested to estimate the amounts of potentially mineralizable organic carbon (PMC) and nitrogen (PMN) as well as recalcitrant organic carbon (ROC) and nitrogen (RON). Eighty-nine surface soil samples were collected in Thailand, Indonesia and Japan from cropland and forest ecosystems. The fresh soils were incubated for 133 days under constant temperature and moisture conditions, and CO2 emissions and mineral N from the soils were monitored. The PMC and PMN were determined by fitting models to the cumulative curves of the CO2 and mineral N. The ROC and RON were determined by subtracting PMC and PMN from total C and total N, respectively. The soil properties tested included soil pH, sand, silt and clay contents, amounts of the acid oxalate soluble Si, Al and Fe, carbon and nitrogen contents of the light fraction ([LF] < 1.6 g cm−3 ) and heavy fraction (HF), and the C/N ratio of the LF and HF. The meteorological properties considered were mean annual temperature and precipitation. Using multiple regression analysis and a stepwise method, PMC and PMN was well estimated by the carbon and nitrogen content of LF (LFC and LFN) and the clay content. This suggests the partially labile nature of clay-associating organic matter as well as LFC and LFN. The PMC and PMN were well estimated by LFC and LFN in forest soils and clay contents in cropland soils. Major factors controlling ROC and RON were light fraction-organic matter, amorphous materials and clay content, suggesting the importance of parent materials in estimating the amount of recalcitrant organic matter in humid Asia. 相似文献
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The relationship between copper accumulated in vineyard calcareous soils and soil organic matter and iron 总被引：3，自引：0，他引：3
C. Parat b R. Chaussod J. Lévêque S. Dousset & F. Andreux 《European Journal of Soil Science》2002,53(4):663-670
The intensive use for over 100 years of copper sulphate (Bordeaux mixture) to fight mildew in vineyards has led to a substantial accumulation of copper (Cu) in surface soils. To assess the effects of such large concentrations, the surface soils of 10 Burgundy vineyards were sampled and analysed for total organic matter (carbon and nitrogen) and metal (copper and iron) contents. Physical (i.e. size fractionation) and chemical (sequential extraction) methods were used to determine the distribution of these elements. The most Cu‐contaminated plots showed the largest accumulation of organic carbon and Cu in the coarse sand and fine sand fractions. Copper was strongly correlated with organic carbon and organic nitrogen in the coarse sand fraction and with organic nitrogen in the fine sand fraction. Copper was also highly correlated with both Fe and organic nitrogen in the clay fraction but not significantly with organic carbon. The sequential extraction showed that Cu was bound mainly to the Fe oxides. However, in the most Cu‐contaminated plots, a part of added Cu was bound to organic matter. This study suggests that Cu protected indirectly the organic matter present in the coarse fractions against biodegradation, and therefore modified the distribution of organic carbon among the particle‐size fractions. Iron appeared as the main factor responsible for Cu accumulation in the clay fraction, mainly through inclusion of Cu in Fe oxyhydroxides and possibly in clay–humus complexes. 相似文献
13.
The influence of tillage treatment and the time of crust formation after planting on the degree of surface crusting and seedling emergence of soybean (Glycine max L. Merr.), planted on the flat and on ridges, are described. Crusts were developed artificially at specific times after planting. Under non-crusted conditions (control), more rapid drying of the soil in the seed zone occurred in conventionally-tilled, ridge-planted (Tcr) and minimum-tilled, flat-planted (Tmf) seedbeds compared with excessively and conventionally-tilled, flat-planted (Tef and Tcf) seedbeds. The formation of surface crusts induced a reduction in moisture loss from the seed zone. On drying, large crust blocks with a smooth surface developed in Tef plots whereas, in Tmf plots, small crust blocks with a rough surface appeared. Both the rate of emergence and the ultimate emergence of soybeans were in the order Tef > Tcf > Tcr > Tmf under non-crusted conditions and, on average, in the order Tcr > Tcf > Tef > Tmf under crusted conditions. Crusts which formed within two days of sowing were more injurious because these were hard and impenetrable, and were present at the normal time of seedling emergence. Crusts induced 72 h after planting had less effect on seedling emergence because, by the time they could form, emergence was already almost completed. 相似文献
14.
Kiyoshi Tsutsuki Chikage Suzuki Shozo Kuwatsuka Peter Becker-Heidmann Hans-Wilhelm Scharpenseel 《植物养料与土壤学杂志》1988,151(2):87-90
Soil organic matter in Mollisols is often preserved for an extremely long period (e.g. > 3000 years). We confirmed that the stable organic matter in Mollisols is the medium to coarse sized (0.2–2.0 μm) clay-humus complex with humic acid combined with calcium as the main organic constituent. The argillic horizon contained relatively large amounts of clay-humus complexes and had relatively high carbon contents, humic acid/fulvic acid ratios and degrees of humification of humic acid. Medium clay and coarse clay fractions preserved the organic carbon most efficiently. Highly humified humic acid could be detected even in the uppermost part of the Ah horizon and was probably stabilized in lower horizons by forming a complex with clay fractions. 相似文献
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改良剂对复垦土壤团聚体组成及有机碳含量的影响 总被引：1，自引：0，他引：1
为探究改良剂对复垦土壤团聚体组成及有机碳含量的影响,采用田间微区的方法按表层0—20 cm土壤重量占比1%,3%,5%的比例添加泥炭、腐殖酸和蛭石,研究3种改良剂对复垦土壤团聚体组成、总有机碳、各粒级团聚体有机碳含量、土壤红外光谱特征的影响。结果表明:施用3种改良剂后各处理土壤机械稳定性团聚体均以>5 mm的最多,施用泥炭和腐殖酸后>5 mm团聚体含量随着改良剂施用比例的升高而增大,且MWD(平均质量直径)值均高于CK。其中,5%腐殖酸对调控>5 mm团聚体含量效果最佳,在6个月时>5 mm机械稳定性团聚体占比达到60.03%。而施用蛭石后>5 mm机械稳定性团聚体的占比与CK相比有所下降。施用3种改良剂后土壤水稳性团聚体以<0.053 mm团聚体含量最高,但其含量均随改良剂施用比例的升高而降低。泥炭和腐殖酸能够提高复垦土壤总有机碳的含量,增强抗侵蚀能力和团聚体的稳定性,而施用蛭石后有机碳含量减少。泥碳、腐殖酸和蛭石各处理下各粒级机械稳定性团聚体有机碳含量均以>5 mm最高,0.053~0.25 mm次之,<0.053 mm最少,有机碳含量贡献率也以>5 mm团聚体的最大,泥炭和腐殖酸处理下>5 mm团聚体有机碳含量贡献率均高于50%,<0.053 mm团聚体有机碳贡献率仅有0.63%~2.82%。从土壤的红外光谱特征峰可以看出,施用腐殖酸能够增加土壤中的多糖类物质,而多糖类物质有大量的—OH,能与黏粒矿物晶面上的氧原子形成氢键而把土粒团聚起来。 相似文献
16.
D.J. LINEHAN 《European Journal of Soil Science》1978,29(3):373-377
Water-ex tractable poly carboxy lie acids and alkali-extractable humic acids and fulvic acids, were isolated from agricultural top-soils of two soil associations. Samples from four soil series from each association were selected with drainage status varying from well-drained to very poorly-drained. The amounts of atkali-extractable humic acid and water-ex tractable polycarboxylic acids were highest in the very poorly-drained soils whilst the amounts of alkali-extractable fulvic acid were generally similar in all the soils, although the fulvic acid accounted for a lower proportion of the total organic matter in the poorly-drained soils. Oxalate-extractable aluminium decreased with increased drainage impedance, whilst no such trend was observed for oxalate-extractable iron. It is suggested that the fulvic acid-like polycarboxylic acids are removed from the soil solution by adsorption onto sesquioxides; so that the lower content of aluminium oxides in the very poorly-drained soils results in depressed levels of fulvic acid and increased concentrations of water-extractable polycarboxylic acids. 相似文献
17.
G. L. B. Wiesenberg L. Schwark & M. W. I. Schmidt 《European Journal of Soil Science》2006,57(5):634-643
Chemical alteration of plant biomass to soil organic matter is often accompanied by characteristic trends, e.g. with decreasing particle size and increasing depth organic carbon and nitrogen concentrations and stable carbon isotope values (δ13C) often increase. In agricultural soils, systematic studies of soil organic carbon (SOC) distribution in bulk soils and particle‐size separates of depth profiles are scarce. In this study, three soil profiles from one site with different monoculture crops were analysed for organic carbon and nitrogen concentrations, stable carbon isotopes, bulk extractable lipids, and soil colour. In contrast to most previous observations, stable carbon isotope values were constant over soil depth and within particle‐size separates, probably as a result of little biomass input due to the harvesting techniques applied and the presence of fossil carbon. Bulk extractable lipids contributed 1–10% to the total SOC. Significantly more lipids could be extracted from rye‐ than from maize‐derived SOC. Lipid yields normalized to soil mass increased with decreasing particle size and decreased with depth. When normalized to organic carbon concentration, sand‐size fractions had the largest lipid yields. Soil colour, expressed as Munsell values, was lightest in sand‐ and silt‐size separates. A cross‐plot of Munsell values and their SOC concentrations revealed characteristic, non‐overlapping areas for each particle‐size class and the bulk soils. Clay‐size separates and bulk soils were almost identical in Munsell values, although for clay‐size separates SOC concentrations were much larger than for bulk soils. Thus, the SOC‐rich clay‐size separates exerted the dominant influence on the colour of the bulk soils. Determination of colour and extractable lipid contents could be useful additional parameters for soil characterization. 相似文献
18.
Concentrations of inositol mono-, di- and tri-, tetra-, penta- and hexaphosphate ranged from 5.0 to 12.5, 10.0 to 27.6, 20.0 to 45.0, 22.5 to 64.6, and 20.0 to 275.4 ppm, respectively, in samples of soils that were poorly drained and mostly derived from alluvium. Multiple correlation suggested that the amounts of esters of inositol phosphate other than inositol monophosphate were significantly correlated with organic phosphorus, total phosphorus, organic carbon, total nitrogen, inositol phospate, clay, exchangeable iron and aluminium, and pH. Individually, inositol hexa-, penta-, and di- and triphosphates were significantly correlated with organic phosphorus, total phosphorus, organic carbon, total nitrogen, inositol phosphate, and exchangeable iron and aluminium; inositol tetraphosphate with organic carbon, total nitrogen, inositol phosphate, and exchangeable iron and aluminium; inositol monophosphate with none. 相似文献
19.
The Atterberg limits and the Proctor compaction test are used by engineers for classifying soils and for predicting stability of building foundations. Field capacity and wilting point (agronomic limits) are used to indicate available water for plant uptake. Few studies have related the engineering criteria to the agronomic ones with regard to compaction hazard for soils. This study investigated the relationships between Atterberg limits, agronomic limits and the critical moisture content (moisture content at Proctor maximum density) for three disturbed soils (sandy loam and clay loam soils from a reclaimed Highvale mine site, and a silt loam soil from a grazing site at Lacombe) of different textures. Relationships between bulk density, moisture content and penetration resistance for these soils were also investigated. For the sandy loam and loam soils, the field capacity was close to the critical moisture content but lower than the plastic limit. Therefore, cultivation of these two soils at moisture contents close to field capacity should be avoided since maximum densification occurs at these moisture contents. Overall, the critical moisture content or field capacity would be a better guide for trafficking of sandy loam and loam textured soils than the Atterberg limits. For the clay loam, field capacity was within the plastic range. Thus trafficking this soil at field capacity would cause severe compaction. In conclusion, either field capacity or plastic limit, whichever is less, can be used as a guide to avoid trafficking at this moisture content and beyond. For the sandy loam and loam soils penetration resistance significantly increased only with increased bulk density (P≤0.05). For the clay loam soil, penetration resistance was positively related to bulk density and negatively related to moisture content. 相似文献
20.
草覆盖影响了沙地土壤的水文物理学参数和水流的异质性 总被引：2，自引：0，他引：2
Vegetation cover has a major effect on water flow in soils.Two sites,separated by distance of about 50 m,were selected to quantify the influence of grass cover on hydrophysical parameters and heterogeneity of water flow in a sandy soil emerging during a heavy rain following a long hot,dry period.A control soil(pure sand)with limited impact of vegetation or organic matter was obtained by sampling at 50 cm depth beneath a glade area,and a grassland soil was covered in a 10 cm thick humic layer and colonised by grasses.The persistence of water repellency was measured using the water drop penetration time test,sorptivity and unsaturated hydraulic conductivity using a mini disk infiltrometer, and saturated hydraulic conductivity using a double-ring infiltrometer.Dye tracer experiments were used to assess the heterogeneity of water flow,and both the modified method for estimating effective cross section and an original method for assessing the degree of preferential flow were used to quantify this heterogeneity from the images of dyed soil profiles.Most hydrophysical parameters were substantially different between the two surfaces.The grassland soil had an index of water repellency about 10 times that of pure sand and the persistence of water repellency almost 350 times that of pure sand. Water and ethanol sorptivities in the grassland soil were 7% and 43%,respectively,of those of the pure sand.Hydraulic conductivity and saturated hydraulic conductivities in the grassland soil were 5% and 16%of those of the pure sand, respectively.Dye tracer experiments revealed a stable flow with"air-draining"condition in pure sand and well-developed preferential flow in grassland soil,corresponding to individual grass tussocks and small micro-depressions.The grassland soil was substantially more water repellent and had 3 times the degree of preferential flow compared to pure sand.The results of this study reinforce our view that the consequences of any change in climate,which will ultimately influence hydrology,will be markedly different between grasslands and bare soils. 相似文献