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  • 1
    In: Soil Science Society of America Journal, Wiley, Vol. 62, No. 3 ( 1998-05), p. 810-817
    Abstract: Emissions of CH 4 , N 2 O, and CO 2 from soils are the result of a number of biological and physical processes, each influenced by several environmental and management factors exhibiting spatial variability. This study aimed to assess the spatial variability and spatial dependence of CH 4 , N 2 O, and CO 2 emissions and their underlying soil processes and properties from grasslands on drained peat soil (Terric Histosol). Emissions and possible controlling factors were measured at a field location in Sweden. Measurements were done on two adjacent sites on peat soil on two successive days for each site. Spatial variability was analyzed with trend analysis and variograms. Both sites consumed small amounts of atmospheric CH 4 , i.e., 0.03 and 0.05 mg CH 4 m −2 d −1 , and emitted N 2 O and CO 2 , i.e., 5 to 19 mg N 2 O m −2 d −1 and 4 to 6 g CO 2 m −2 d −1 . Spatial variability of emissions was high, with coefficients of variation of 50 to 1400%. Emissions either showed a spatial trend or were spatially dependent with ranges of spatial dependence of 50 to 〉 200 m. However, spatial dependence of emissions showed differences between sites and short‐term temporal variability. Variograms of emissions and soil processes, which are partly biological in nature and have a high degree of inherent variability, should be interpreted with care.
    Type of Medium: Online Resource
    ISSN: 0361-5995 , 1435-0661
    RVK:
    Language: English
    Publisher: Wiley
    Publication Date: 1998
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  • 2
    Online Resource
    Online Resource
    Elsevier BV ; 1998
    In:  CATENA Vol. 33, No. 3-4 ( 1998-11), p. 139-153
    In: CATENA, Elsevier BV, Vol. 33, No. 3-4 ( 1998-11), p. 139-153
    Type of Medium: Online Resource
    ISSN: 0341-8162
    RVK:
    Language: English
    Publisher: Elsevier BV
    Publication Date: 1998
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  • 3
    Online Resource
    Online Resource
    Elsevier BV ; 2004
    In:  Quaternary Science Reviews Vol. 23, No. 14-15 ( 2004-7), p. 1627-1636
    In: Quaternary Science Reviews, Elsevier BV, Vol. 23, No. 14-15 ( 2004-7), p. 1627-1636
    Type of Medium: Online Resource
    ISSN: 0277-3791
    RVK:
    Language: English
    Publisher: Elsevier BV
    Publication Date: 2004
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  • 4
    Online Resource
    Online Resource
    Cambridge University Press (CUP) ; 1903
    In:  Journal of the Royal Asiatic Society Vol. 35, No. 4 ( 1903-10), p. 735-760
    In: Journal of the Royal Asiatic Society, Cambridge University Press (CUP), Vol. 35, No. 4 ( 1903-10), p. 735-760
    Abstract: The early Persian document written in Hebrew characters which Professor D. S. Margoliouth has at my request kindly undertaken to publish, and of which his present ṗaper is intended to furnish a preliminary account, was obtained by me in the course of my journey of archaeological exploration in Chinese Turkestan carried out during 1900–1, under the orders of the Government of India.
    Type of Medium: Online Resource
    ISSN: 1356-1863 , 1474-0591
    RVK:
    Language: English
    Publisher: Cambridge University Press (CUP)
    Publication Date: 1903
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  • 5
    In: Sedimentology, Wiley, Vol. 65, No. 4 ( 2018-06), p. 993-1042
    Abstract: Reconstruction of the palaeoenvironmental context of Martian sedimentary rocks is central to studies of ancient Martian habitability and regional palaeoclimate history. This paper reports the analysis of a distinct aeolian deposit preserved in Gale crater, Mars, and evaluates its palaeomorphology, the processes responsible for its deposition, and its implications for Gale crater geological history and regional palaeoclimate. Whilst exploring the sedimentary succession cropping out on the northern flank of Aeolis Mons, Gale crater, the Mars Science Laboratory rover Curiosity encountered a decametre‐thick sandstone succession, named the Stimson formation, unconformably overlying lacustrine deposits of the Murray formation. The sandstone contains sand grains characterized by high roundness and sphericity, and cross‐bedding on the order of 1 m in thickness, separated by sub‐horizontal bounding surfaces traceable for tens of metres across outcrops. The cross‐beds are composed of uniform thickness cross‐laminations interpreted as wind‐ripple strata. Cross‐sets are separated by sub‐horizontal bounding surfaces traceable for tens of metres across outcrops that are interpreted as dune migration surfaces. Grain characteristics and presence of wind‐ripple strata indicate deposition of the Stimson formation by aeolian processes. The absence of features characteristic of damp or wet aeolian sediment accumulation indicate deposition in a dry aeolian system. Reconstruction of the palaeogeomorphology suggests that the Stimson dune field was composed largely of simple sinuous crescentic dunes with a height of ca 10 m, and wavelengths of ca 150 m, with local development of complex dunes. Analysis of cross‐strata dip azimuths indicates that the general dune migration direction and hence net sediment transport was towards the north‐east. The juxtaposition of a dry aeolian system unconformably above the lacustrine Murray formation represents starkly contrasting palaeoenvironmental and palaeoclimatic conditions. Stratigraphic relationships indicate that this transition records a significant break in time, with the Stimson formation being deposited after the Murray formation and stratigraphically higher Mount Sharp group rocks had been buried, lithified and subsequently eroded.
    Type of Medium: Online Resource
    ISSN: 0037-0746 , 1365-3091
    URL: Issue
    RVK:
    Language: English
    Publisher: Wiley
    Publication Date: 2018
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  • 6
    Online Resource
    Online Resource
    Wiley ; 1992
    In:  Soil Science Society of America Journal Vol. 56, No. 1 ( 1992-01), p. 187-192
    In: Soil Science Society of America Journal, Wiley, Vol. 56, No. 1 ( 1992-01), p. 187-192
    Abstract: Spatial variation of soil profiles disturbed by leveling was inventoried on a field scale to obtain representative data for simulation purposes. Depth of occurrence, thickness, and morphology of functional layers, which are different pedogenetic horizons with comparable soil physical properties, were considered to be regionalized variables. The layers served as carriers of physical information, such as water‐retention and hydraulic‐conductivity characteristics and organic‐matter content. An impression of the variability within each layer was obtained by six fold sampling. Spatial variability, expressed by variations in thickness of functional layers, was inventoried in a two‐step soil survey. First, semivariograms were constructed using data obtained following a nested sampling scheme supplemented by a nugget estimation procedure. Variograms were used to evaluate cost/quality ratios at varying potential grid sampling densities, using the root of the prediction error variance (RPEV) to compare quality of interpolations. Based on these evaluations and a sequential sampling test, a grid mesh of 12 m was chosen. Second, a grid soil survey and an independent quality test were done, in which root mean square errors (RMSE) on test points were compared with RPEV. The RPEV to RMSE ratios varied between 0.7 and 1.1 for the sampled grid mesh, and had comparable values for other grid meshes. Estimations on test points by an hypothesized spatial mean, based on 26 measurements by a sequential sampling method, produced RMSE values not significantly different from RMSE values from kriging interpolations. However, sequential sampling required 26 observations whereas kriging required 153, a saving of 83%.
    Type of Medium: Online Resource
    ISSN: 0361-5995 , 1435-0661
    RVK:
    Language: English
    Publisher: Wiley
    Publication Date: 1992
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    detail.hit.zdb_id: 2239747-4
    detail.hit.zdb_id: 196788-5
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  • 7
    Online Resource
    Online Resource
    Wiley ; 1988
    In:  Soil Science Society of America Journal Vol. 52, No. 5 ( 1988-09), p. 1418-1423
    In: Soil Science Society of America Journal, Wiley, Vol. 52, No. 5 ( 1988-09), p. 1418-1423
    Abstract: Existing computer calculations by simulation of the moisture deficit (MD) were used for 500 point observations in an area of 404 ha with sandy soils in the Netherlands. The statistical prediction techniques kriging and cokriging were used to predict MD‐values in 100 points selected at random from the 500 available points. The MD‐data at the remaining 400 points were used for the predictions. The mean variance of prediction error (MVPE) and the mean squared error of prediction (MSEP) decreased only slightly when kriging is compared with cokriging using the mean highest water‐table level as a covariable. The number of MD‐values used in cokriging could, however, be reduced from 400 to 160 with only a small loss of accuracy in using 400 observations on the mean highest water‐table (MHW) as a covariable. As the MD‐variables being considered are four times as expensive to determine as the covariable, which is routinely estimated during soil survey, this also represents a considerable reduction of costs. Cokriging can thus be a useful technique to more effectively utilize available soil survey information.
    Type of Medium: Online Resource
    ISSN: 0361-5995 , 1435-0661
    RVK:
    Language: English
    Publisher: Wiley
    Publication Date: 1988
    detail.hit.zdb_id: 241415-6
    detail.hit.zdb_id: 2239747-4
    detail.hit.zdb_id: 196788-5
    detail.hit.zdb_id: 1481691-X
    SSG: 13
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  • 8
    Online Resource
    Online Resource
    Wiley ; 1992
    In:  Soil Science Society of America Journal Vol. 56, No. 2 ( 1992-03), p. 525-531
    In: Soil Science Society of America Journal, Wiley, Vol. 56, No. 2 ( 1992-03), p. 525-531
    Abstract: In most soil surveys, and particularly those carried out in developing countries, the bulk of recorded soil data is on an ordinal measurement scale. This determines the type of statistics and techniques that can be used for data processing. For example, with ordinal data the mode, median, and range can be used as summary statistics. For describing the spatial structure of ordinal data we propose the spatial‐difference‐probability function, which is comparable with the semivariogram. From a soil survey in Costa Rica, three different suitability maps for banana ( Musa x paradisiaca L.) were produced according to a qualitative land‐evaluation procedure by interpreting: (i) the 1:200 000 soil map, (ii) the 1:50 000 soil map, and (iii) point data. The quality of these three maps was tested by looking at the reliability, relevance, and presentation of information, using 98 test borings. Reliability was characterized in terms of purity and range. The suitability map based on the 1:200 000 soil map was the most reliable one, with an overall purity of 49%. The suitability map produced by interpolating point data was the most relevant one, as defined in terms of the possibility to correctly identify potential locations for banana plantations from the map. Differences in presentation of information were evaluated by comparing the boundary indices of the different maps. The suitability map based on the 1:50 000 soil map was the most readable one. Map choice should be based on a consideration by the user of the different quality criteria.
    Type of Medium: Online Resource
    ISSN: 0361-5995 , 1435-0661
    RVK:
    Language: English
    Publisher: Wiley
    Publication Date: 1992
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    SSG: 13
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  • 9
    Online Resource
    Online Resource
    Cambridge University Press (CUP) ; 1900
    In:  Journal of the Royal Asiatic Society of Great Britain & Ireland Vol. 32, No. 2 ( 1900-04), p. 187-194
    In: Journal of the Royal Asiatic Society of Great Britain & Ireland, Cambridge University Press (CUP), Vol. 32, No. 2 ( 1900-04), p. 187-194
    Abstract: The manuscript to which the present note refers was purchased by me at Śrīnagar in October, 1898. It is written in Śāradā characters, and contains the Gada, Sauptika, Strī, and Aśvamedha Parvans of the Mahābhārata. The manuscript acquired by me originally formed only a portion of a codex which must have contained the whole of the great Sanskrit epic. This is made clear by the curious notice I shall proceed to discuss, as well as by the fact that other portions of the codex have been seen by me in Śrīnagar during earlier visits. The whole must have formed two large folio volumes which, judging from the writing and the paper, were probably copied in the sixteenth century, or in the early part of the seventeenth. The manuscript is very carefully written, evidently by the hand of a Paṇḍit, and represents a very good specimen of the text of the Western recension of the Mahābhārata current in Kaśmīr.
    Type of Medium: Online Resource
    ISSN: 0035-869X , 2051-2066
    RVK:
    Language: English
    Publisher: Cambridge University Press (CUP)
    Publication Date: 1900
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  • 10
    In: Quaternary Science Reviews, Elsevier BV, Vol. 27, No. 25-26 ( 2008-12), p. 2426-2441
    Type of Medium: Online Resource
    ISSN: 0277-3791
    RVK:
    Language: English
    Publisher: Elsevier BV
    Publication Date: 2008
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