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標(biāo)題: Titlebook: Environmental Geology; Handbook of Field Me Klaus Kn?del,Gerhard Lange,Hans-Jürgen Voigt Book 2007 Springer-Verlag Berlin Heidelberg 2007 B [打印本頁]

作者: FLUX    時(shí)間: 2025-3-21 17:18
書目名稱Environmental Geology影響因子(影響力)




書目名稱Environmental Geology影響因子(影響力)學(xué)科排名




書目名稱Environmental Geology網(wǎng)絡(luò)公開度




書目名稱Environmental Geology網(wǎng)絡(luò)公開度學(xué)科排名




書目名稱Environmental Geology被引頻次




書目名稱Environmental Geology被引頻次學(xué)科排名




書目名稱Environmental Geology年度引用




書目名稱Environmental Geology年度引用學(xué)科排名




書目名稱Environmental Geology讀者反饋




書目名稱Environmental Geology讀者反饋學(xué)科排名





作者: CREEK    時(shí)間: 2025-3-21 23:42
Borehole Loggingved from the data. Measurements on the cores themselves are also sometimes made. Borehole logging has certain advantages with respect to core measurements. For example, in a hole where there is limited core recovery, the depth of the incomplete cores can be uncertain; logs provide a continuous depth
作者: 建筑師    時(shí)間: 2025-3-22 01:51
Data Fusionof data fusion in use, depending on the degree of knowledge extraction and representation. In pixel-level fusion, the data (e.g., images) from different sensors are combined at the pixel level. In attribute-level fusion, the features and objects are extracted from different representations (e.g., im
作者: 拉開這車床    時(shí)間: 2025-3-22 08:38
https://doi.org/10.1007/978-3-662-36304-1ved from the data. Measurements on the cores themselves are also sometimes made. Borehole logging has certain advantages with respect to core measurements. For example, in a hole where there is limited core recovery, the depth of the incomplete cores can be uncertain; logs provide a continuous depth
作者: 品嘗你的人    時(shí)間: 2025-3-22 11:20
,Zwei weitere F?lle von Hepatomegalie,of data fusion in use, depending on the degree of knowledge extraction and representation. In pixel-level fusion, the data (e.g., images) from different sensors are combined at the pixel level. In attribute-level fusion, the features and objects are extracted from different representations (e.g., im
作者: APNEA    時(shí)間: 2025-3-22 15:20

作者: APNEA    時(shí)間: 2025-3-22 19:20
Book 2007ty has become more aware of, and concerned about, stewardship of the natural environment – water, soil, and air. Sustainable development has become more widely received and promoted in many parts of the world. The need is now critical for earth and environmental scientists and engineers to work toge
作者: 無力更進(jìn)    時(shí)間: 2025-3-23 00:00

作者: absolve    時(shí)間: 2025-3-23 01:40

作者: VOK    時(shí)間: 2025-3-23 06:40

作者: 發(fā)牢騷    時(shí)間: 2025-3-23 12:58
https://doi.org/10.1007/978-3-658-27383-5r, middle, and thermal infrared (Table 3.1-1). MSS can work in rather narrow spectral bands of a few nanometers. Thus, such remote sensing can focus on specific spectral features to identify detailed physical and chemical characteristics of the land surface objects of interest.
作者: 胎兒    時(shí)間: 2025-3-23 14:08

作者: 咽下    時(shí)間: 2025-3-23 20:04

作者: 儲(chǔ)備    時(shí)間: 2025-3-24 00:40

作者: BROOK    時(shí)間: 2025-3-24 02:31
row and the detrimental aftereffects of industrialization and environmental negligence become more apparent, society has become more aware of, and concerned about, stewardship of the natural environment – water, soil, and air. Sustainable development has become more widely received and promoted in m
作者: 不要不誠實(shí)    時(shí)間: 2025-3-24 08:49

作者: 厚顏    時(shí)間: 2025-3-24 14:16
https://doi.org/10.1007/978-3-658-41574-7d spatial patterns and associations. Hence, such observations can be interpreted and analyzed with regard to their geoscientific information (Chapter 3.1) and with regard to their geometric structures (Chapter 3.2).
作者: 航海太平洋    時(shí)間: 2025-3-24 17:47
https://doi.org/10.1007/978-3-540-88647-1 the Earth’s magnetic field ranging from 10. seconds to several hours to study the distribution of the conductivities with depth (Cagniard, 1953). The electromagnetic exploration methods described in this Chapter are based on the use of electromagnetic fields generated by controlled sources.
作者: Fierce    時(shí)間: 2025-3-24 22:24
Nonphotographic Imaging from Aircraft and Space-borne Platformsr, middle, and thermal infrared (Table 3.1-1). MSS can work in rather narrow spectral bands of a few nanometers. Thus, such remote sensing can focus on specific spectral features to identify detailed physical and chemical characteristics of the land surface objects of interest.
作者: 陳腐的人    時(shí)間: 2025-3-25 00:45
Gravity Methodsocal gravity field differences due to density variations in the subsurface. The effects of smallscale masses are very small compared with the effects of the global part of the Earth’s gravity field (often on the order of 1 part in 10. to 10.).
作者: 心神不寧    時(shí)間: 2025-3-25 05:45

作者: buoyant    時(shí)間: 2025-3-25 10:28

作者: DENT    時(shí)間: 2025-3-25 15:29
https://doi.org/10.1007/978-3-658-40546-5y) in the ground. As the potential between P. and P., the current introduced through C. and C., and the electrode configuration are known, the resistivity of the ground can be determined; this is referred to as the “apparent resistivity”.
作者: Pelvic-Floor    時(shí)間: 2025-3-25 18:37
Studien zur KommunikationswissenschaftES) for ice thickness measurements on polar ice sheets. The method was first applied by . (1929), . in Austria to estimate the thickness of a glacier. GPR has been increasingly accepted for geological, engineering, environmental, and archaeological investigations since the 1980s.
作者: Phonophobia    時(shí)間: 2025-3-25 23:13

作者: 蟄伏    時(shí)間: 2025-3-26 03:13
Direct Current Resistivity Methodsy) in the ground. As the potential between P. and P., the current introduced through C. and C., and the electrode configuration are known, the resistivity of the ground can be determined; this is referred to as the “apparent resistivity”.
作者: 鍵琴    時(shí)間: 2025-3-26 07:28
Ground Penetrating RadarES) for ice thickness measurements on polar ice sheets. The method was first applied by . (1929), . in Austria to estimate the thickness of a glacier. GPR has been increasingly accepted for geological, engineering, environmental, and archaeological investigations since the 1980s.
作者: 類似思想    時(shí)間: 2025-3-26 09:01

作者: 無可爭辯    時(shí)間: 2025-3-26 13:23

作者: 殘暴    時(shí)間: 2025-3-26 18:09

作者: 我們的面粉    時(shí)間: 2025-3-26 23:50
https://doi.org/10.1007/978-3-658-41997-4rt 1. The geoscientific methods are described in more detail in Parts 3 to 5. Certain preparations are required for any site investigation using ground-based methods in order to ensure the efficient implementation of field operations.
作者: 閃光你我    時(shí)間: 2025-3-27 01:47
Warum so viele Offerten vor die Wand fahren,ial photography can address a multitude of geoscientific questions and can be highly effective when used for logistics and planning (., 1992). The cost of aerial photography is rather low. The data are informative, easy to manage, and the film does not require special image processing resources for analysis.
作者: cortex    時(shí)間: 2025-3-27 08:06

作者: phase-2-enzyme    時(shí)間: 2025-3-27 09:49

作者: Invertebrate    時(shí)間: 2025-3-27 17:32
Preparatory Steps and Common Problemsrt 1. The geoscientific methods are described in more detail in Parts 3 to 5. Certain preparations are required for any site investigation using ground-based methods in order to ensure the efficient implementation of field operations.
作者: 懸掛    時(shí)間: 2025-3-27 18:39

作者: Gum-Disease    時(shí)間: 2025-3-27 23:54

作者: Gnrh670    時(shí)間: 2025-3-28 03:38
Geophysical In-situ Groundwater and Soil Monitoringants. The integrity of contaminant barriers and the success of rehabilitation of contaminated sites must also be monitored. The spread of contaminants occurs via three paths: water, soil, and air. Of these, groundwater and surface water are the most significant.
作者: 糾纏,纏繞    時(shí)間: 2025-3-28 09:29

作者: Mortal    時(shí)間: 2025-3-28 13:37

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作者: 有偏見    時(shí)間: 2025-3-28 21:50

作者: 燒瓶    時(shí)間: 2025-3-29 01:15
https://doi.org/10.1007/978-3-658-27383-5 or special antennas. While photography is limited to a spectral range from 0.3 to 0.9 μm, multispectral scanners (MSS) can operate in wavelength regions from 0.3 to approximately 14 um (Lillesand & Kiefer, 1994; Gupta, 2003). This range includes radiation in the near ultraviolet, visible light, nea
作者: 套索    時(shí)間: 2025-3-29 05:23
https://doi.org/10.1007/978-3-662-61613-0cribed by Newton’s law of universal gravitation. An effect of gravity is observed when the fruit from a tree falls to the ground. The gravity field at each location on Earth consists of a global field which is superimposed by a local anomaly field. In a gravity survey, measurements are made of the l
作者: Infiltrate    時(shí)間: 2025-3-29 08:13
https://doi.org/10.1007/978-3-658-40546-5ivity methods, a current is introduced into the ground through point electrodes (C., C.) and the potential field is measured using two other electrodes (the potential electrodes P. and P.), as shown in .. The source current can be direct current or low-frequency (0.1 – 30 Hz) alternating current. Th
作者: 繁殖    時(shí)間: 2025-3-29 11:46

作者: 平庸的人或物    時(shí)間: 2025-3-29 17:37

作者: 紳士    時(shí)間: 2025-3-29 22:43
https://doi.org/10.1007/978-3-322-82116-4al parameters of an aquifer can be determined directly. In contrast to SNMR, other geophysical techniques, e.g., dc resistivity soundings (VES), electromagnetics, seismics, and ground penetrating radar only provide information on the lithological character of aquifers and aquicludes indirectly.
作者: Foregery    時(shí)間: 2025-3-30 03:34
https://doi.org/10.1007/978-3-662-36304-1 parameter values and petrographic data can be obtained from them in the laboratory. For technical and economic reasons, however, drill cores are not taken from every borehole. Borehole logging (also called well logging or downhole logging) provides in-situ information in addition to the direct geol
作者: Morose    時(shí)間: 2025-3-30 04:02
Elastische Schwingungen und Wellen,ants. The integrity of contaminant barriers and the success of rehabilitation of contaminated sites must also be monitored. The spread of contaminants occurs via three paths: water, soil, and air. Of these, groundwater and surface water are the most significant.
作者: cutlery    時(shí)間: 2025-3-30 08:35
https://doi.org/10.1007/978-3-642-99336-7nto account: stratigraphic sequence, thickness and lateral extent of strata and other geological units, lithology, homogeneity and heterogeneity, bedding conditions, tectonic structures, fractures, and impact of weathering. Information about landforms (geomorphology), earthquake risk, activity of fa
作者: patriot    時(shí)間: 2025-3-30 14:46

作者: ALIEN    時(shí)間: 2025-3-30 20:12

作者: 過度    時(shí)間: 2025-3-31 00:38

作者: GULF    時(shí)間: 2025-3-31 01:01

作者: PALMY    時(shí)間: 2025-3-31 07:16
Pflanzenphysiologische PraktikaAlmost all data obtained in geoscientific investigations need some kind of statistical treatment for interpretation, as well as for the assessment of reliability and errors. The following statistical methods are frequently used to analyze data sets:
作者: Absenteeism    時(shí)間: 2025-3-31 13:14

作者: 宏偉    時(shí)間: 2025-3-31 13:46

作者: Distribution    時(shí)間: 2025-3-31 18:49
Springer-Verlag Berlin Heidelberg 2007
作者: 純樸    時(shí)間: 2025-3-31 22:29

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