Subsoil Sentence Examples

subsoil
  • It rests on a subsoil of clay and marl.

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  • As the drainage by cuniculi removed the moisture in the subsoil, so the drainage of the lakes by emissaria, outlet channels at a low level, prevented the permeable strata below the tufa from becoming impregnated with moisture which they would otherwise have derived from the lakes of the Alban Hills.

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  • Here the prevailing soils are grey and sandy with a subsoil of loam, but they are less fertile than those of the Lime Sink or Cotton Belts.

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  • The subsoil is either of clay, of limestone, or mixed sand and clay, gravel, or of a peculiar kind of pudding stone which exists in a hard and a soft variety.

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  • Except on extremely heavy soils or on shallow soils with a subsoil which it is unwise to bring upon the surface, the modern tendency is in favour of the digging plough.

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  • In winter, however, and in fallows loss takes place in the subsoil water.

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  • It is suitable for stiffish soils where the subsoil is fairly open, but is less successful in sand.

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  • The nature of the subsoil is of scarcely less importance than that of the surface soil.

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  • The planting of eucalyptus trees is out of favour at present, but it appears to have been successful in Portugal, not from any prophylactic virtues in the plant, but through the great absorption of moisture by its deep roots, which tends to dry the subsoil.

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  • These prairies are traversed by ridges, which facilitate irrigation, and are underlaid by an impervious subsoil, which facilitates both effective storage and drainage.

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  • Below this is the subsoil.

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  • The subsoil not unfrequently contains materials which are deleterious to the growth of crops, and roots descending into it may absorb and convey these poisonous substances to other parts of the plant or be themselves damaged by contact with them.

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  • On this account deeper tillage than usual, which allows of easier penetration of roots, or the carrying out of operations which bring the subsoil to the surface, must always be carefully considered.

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  • Mexico was formerly one of the worst drained large cities of the New World, its subsoil being permanently saturated and its artificial drainage being through open ditches into the San Lazaro Canal which nominally discharged into Lake Texcoco.

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  • The surface soil is clay in which are embedded fragments of siliceous sandstone, used for millstones and constructional purposes; the subsoil is limestone.

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  • Many gardeners are still afraid to disturb an unsuitable subsoil, but experienced growers have proved that by bringing it up to the surface and placing plenty of manure in the bottoms of the various trenches, the very best results are attained in the course of a season or so.

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  • An uneven subsoil, especially if retentive, is most undesirable, as water is apt to collect in the hollows, and thus affect the upper soil.

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  • When the subsoil is too compact to be pervious to water, effectual drainage must be resorted to; when it is very loose, so that it drains away the fertile ingredients of the soil as well as those which are artificially supplied, the compactness of the stratum should be increased by the addition of clay, marl or loam.

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  • A pit of this character may be sunk into the ground deeper than is indicated in the figure if the subsoil is dry and gravelly, but in the case of a damp subsoil it should rather be more elevated, as the soil could easily be sloped up to meet the retaining wall.

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  • In the second case all roots that have struck downwards into a cold uncongenial subsoil must be pruned off if they cannot be turned in a lateral direction, and all the lateral ones that have become coarse and fibreless must also be shortened back by means of a clean cut with a sharp knife, while a compost of rich loamy soil with a little bone-meal, and leaf-mould or old manure, should be filled into the trenches from which the old sterile soil has been taken.

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  • Many of them also grow satisfactorily in a peaty soil if well worked, especially if they have a cool moist subsoil.

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  • The bottom of the border as well as that Cymbidium Cypripedium Cyrtopodium Dendrobium Diacrium Disa Epidendrum Eulophia Eulophiella Galeandra Gongora Grammatophyllum Habenaria Houlletia lonopsis Ipsea Laelia Laelio-Cattleya* Leptotes Lissochilus Lycaste Masdevallia Miltonia Mormodes Odontoglossum Odontioda* Oncidium Peristeria Pescatorea Phaj us Phaio - calanthe* Phalaenopsis Pilumna Platyclinis Pleione Pleurothallis Polystachya Promenaea Renanthera Restrepia Rodriguezia S accolabium Schomburgkia Scuticaria Sobralia Sophro-cattleya* Sophronitis Spathoglottis Stanhopea Thunia Trichopilia Trichosma Vanda Zygo - colax* of the drain must be kept lower than the general level of the subsoil, else the soakage will gather in all the little depressions of its surface.

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  • Amongst causes of variation in the quantity of water needed will be its quality and temperature and rate of flow, the climate, the season, the soil, the subsoil, the artificial drainage, the slope, the aspect and the crop. In actual practice the amount of water varies from 300 gallons per acre in the hour to no less than 28,000 gallons.

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  • In this way as the water sinks down through the porous subsoil or into the subterranean drains oxygen enters and supplies an element which is needed, not only for the oxidation of organic matters in the earth, but also for the direct and indirect nutrition of the roots.

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  • The Famine Commission of 1878 urged the importance of forest conservancy as a safeguard to agriculture, pointing out that a supply of wood for fuel was necessary if cattle manure was to be used to any extent for the fields, and also that forest growth served to retain the moisture in the subsoil.

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  • It thrives most in a light loam with a dry subsoil; rich and, in particular, wet soils are unsuitable, conducing to the formation of too much wood.

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  • There seems reason to believe that it refers to the time when the site, or a portion of it, formed an island, as sea-sand is the subsoil even of the oldest quarters.

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  • Flax prospers most when grown upon land of firm texture resting upon a moist subsoil.

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  • Even the beds of sluggish rivers flowing over porous strata generally become so impermeable that excavations made in their neighbourhood, though freely collecting the subsoil water, receive no FIG.

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  • Taramelli (Notizie degli Scavi, 1905, 41 seq.) rightly points out that the nucleus of the Roman municipium is probably represented by the present quarter of the Marina, in which the streets intersect at right angles and Roman remains are frequently found in the subsoil.

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  • Good drainage is essential for drought tolerant plants and so gritty topsoil has been used, mounded up into bunds over rubble filled subsoil.

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  • The backfill was identified as a dark gray clay silt with mixed gravel and lumps of redeposited subsoil.

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  • Within this test pit two deposits were found to overlie the natural subsoil.

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  • Within Blue Bridge Lane, Trench D exposed subsoil at a depth of 0.35m below the present ground surface.

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  • As a result, the deposit sequence within the feature was difficult to differentiate against surrounding subsoil.

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  • The liner should then be covered with a layer of sandy subsoil.

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  • Topsoil stripping revealed a similar surface to that on Area 1. At the southern end there was an orange brown subsoil overlying glacial gravel.

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  • The topsoil came down directly onto the underlying subsoil.

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  • What are the 3 main types of natural subsoil?

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  • The soil slightly varies, but in general it is found to be a dark loamy mold, with a stiff clayey subsoil.

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  • For instance, light sandy topsoil on top of clay subsoil may result in boggy conditions where the two soils meet.

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  • They are mostly filled with sandy material which is much more compact than the gravel subsoil into which they are cut.

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  • With a wet, undrained subsoil and a large population of Indians and half-breeds living in crowded quarters, the death-rate has been notoriously high, though the completion of the Valley drainage works in 1900, supplemented by underground sewers in the better parts of the city, and by better sanitation, have recently improved matters.

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  • The soil consists of clay and loam, with a subsoil of clay.

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  • The soil is sandy, upon a subsoil of gravel.

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  • This method of building extends east as far as Basingstoke where the subsoil used is mainly chalk.

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  • Where the underlying rock or gravel deposits are close to the surface, the subsoil layer may be very thin.

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  • Foundations Designed and constructed to suit local subsoil conditions, and to comply with all current building legislation.

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  • Iron compounds, in various states of oxidation and reduction (hydration) are major coloring agents of subsoil horizons.

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  • Chalk subsoil was, in all areas, cleaned to locate any possible subsurface features.

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  • Compressed heavy clay loam topsoil horizon (102) 0.45 - 0.5m Subsoil.

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  • While there are few soils in which it will not thrive, it prefers such as are light, with a warm gravelly subsoil.

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  • The leaves are larger than those of the Common Box, and when exposed to the sun are of a lighter green, but it only succeeds well in warm, well-sheltered situations, with a dry soil and a warm subsoil.

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  • Their thick fleshy roots thrive in a rich loam, and like a damp subsoil; impatient of removal, and should not be increased by division.

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  • The best position for it is a rather damp spot near a running stream, where the subsoil is always moist.

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  • A well-drained subsoil with a porous surface soil suits them best, and shelter from hard frost and nipping winds is of great service.

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  • If this takes you down into compacted subsoil, remove it.

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  • Add compost and soil amendments mixing them into the subsoil with spading fork.

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  • The subsoil was composed principally of clay and sand, and the railway had to be carried over the moss on the level, requiring cutting, and embanking for upwards of 4 m.

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  • Put comprehensively, it involves the control of the subsoil and surface waters by drainage, the regulation of rivers and floods, suitable agriculture, the clearing of forests or jungles, which tend to increase the rainfall and keep the ground swampy.

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  • In the British Isles wheat is, as a rule, sown in the autumn on a heavier soil, and has four or five months in which to distribute its roots, and so it gets possession of a wide range of soil and subsoil before barley is sown in the spring.

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  • It is deeper and more fertile, however, in the basins of the Great Miami and Little Miami rivers, where there is a liberal mixture of decomposed limestone and where extensive areas with a clay subsoil are covered with alluvial deposits.

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  • On his farm Smith carried out his experiments in deep and thorough draining, and also invented a reaping machine, the subsoil plough and numerous other valuable appliances.

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  • Their growth makes no new addition of mineral food-constituents to the land, but they bring useful substances from the subsoil nearer to the surface, and after the decay of the buried vegetation these become available to succeeding crops of wheat or other plants.

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  • Moreover, where deep-rooting plants are grown the subsoil is aerated and rendered more open and suitable for the development of future crops.

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  • As a group they are cosmopolitan, their northern limit approaching that of the permanently frozen subsoil, while in the southern hemisphere the southern point of Patagonia forms the farthest limit.

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  • In the Piedmont Plateau and Appalachian Mountains Regions the surface soil is generally sandy, but in considerable areas the subsoil is a red clay derived largely from the decomposition of hornblende.

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  • The soft limestone underlying this region is covered, in the uplands, with grey, sandy soils, which have a subsoil of loam; in the lowlands the surface soils are loams, the subsoils clays.

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  • The finest wines of the Medoc and Graves are largely grown on a mixture of gravel, quartz and sand with a subsoil of alios or clay.

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  • The soil is almost a pure sandy gravel with a subsoil of varied nature, but principally altos, gravel, clay or sand.

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  • The effect of this industry, however, is to lay bare a subsoil of diluvial sand which offers little inducement for subsequent cultivation.

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  • Speaking generally, the Ozark region is characterized by reddish clays, mixed with gravels and stones, and cultivable in inverse proportion to the amount of these elements; northern Missouri by a generally black clay loam over a clay subsoil, with practically no admixture of stones; the southern prairies, above referred to, share the characteristics of those north of the Missouri.

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  • In this case, as in that of a level plane of uniformly porous sand, the vertical section of the figure is tangential to the vertical well and to the natural level of the subsoil water.

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  • Land is not in a satisfactory condition with respect to drainage unless the rain that falls upon it can sink down to the minimum depth required for the healthy development of the roots of crops and thence find vent either through a naturally porous subsoil or by artificial channels.

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  • These fine-grained materials are at first mixed with broken and more or less weathered rock fragments and coarser mineral particles in the soil and subsoil, but by the action of wind and rain they are swept away and deposited in distant situations.

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  • On the south bank, owing to better natural drainage and a drier subsoil, movement was fairly easy, but the Austrians found it almost impossible.

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  • The valley of the Medway, especially the district round Maidstone, is the most fertile part of the county, the soil being a deep loam with a subsoil of brick-earth.

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  • The work of earthworms in aiding in the production of the subsoil and in levelling the surface was first studied by C. Darwin, and has since been investigated by others.

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  • It is the leguminous fodder crops-especially clover, which has a much more extended period of growth, and much wider range of collection within the soil and subsoil, than any of the other crops of the rotation-that yield in their produce the largest amount of nitrogen per acre.

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  • In case of adhesive clayey subsoil this can generally be secured by placing over the sloping bottom a good layer of coarse rubbly material, communicating with a drain in front to carry off the water, while earthenware drain tubes may be laid beneath the rubble from 8 to To ft.

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  • In all sections of the Piedmont Plateau the subsoil is a reddish or yellowish clay.

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