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Soil Sampling for Microbiological Analysis 土壤取样微生物分析
Pub Date : 2018-09-11 DOI: 10.2136/SSSABOOKSER5.2.C1
A. G. Wollum
Soil is a unique medium containing a diverse community of organisms, representing many morphological and physiological types. Attempting to numerically characterize these organisms or their activities requires an understanding of both the spatial and temporal distribution of organisms within the soil environment. The fact that organisms in soils are rarely static in numbers or activity, compounds the problem of characterizing populations or their activities. Many organisms exist at relatively low levels numerically but can have a profound affect on nutrient availability, plant development, or environmental quality. In most cases, it is impossible to equate the numbers of a particular organism with its importance in the soil ecosystem. Further, the enumeration of any population or magnitude of activity represents a point-in-time measurement that is at some dynamic equilibrium governed by the physical, chemical, and biological environment. Variability is a familiar problem to most scientists, especially those dealing with environmental issues or habitats. Even the novice soil scientist recognizes that soils differ from site to site, based on observable differences such as color, depth, or arrangement of soil horizons. Less obvious is the fact that not only do the gross soil properties vary from site to site, but within a site, significant variation may occur. Intuitively, one might suspect that microbial populations vary by depth, with the surface horizons generally having more organisms and a greater abundance of types than the subsurface horizons. Information provided by Waksman and Starkey (1931) support this contention. For different soils, organisms were always more numerous in the surface horizons as compared to the subsurface horizons. These differences were attributed to the fact that the physical and chemical properties were different for different layers of soil, thus giving rise to heterogenous distributions of microorganisms. Besides variation within the profile, it is reasonable to expect spatial variation in soil microbiological properties within sampling area smaller
土壤是一种独特的介质,包含了多种多样的生物群落,代表了许多形态和生理类型。试图用数字表征这些生物或它们的活动需要了解土壤环境中生物的空间和时间分布。土壤中的生物在数量或活动上很少是静态的,这一事实使描述种群特征或其活动的问题复杂化。许多生物体存在于相对较低的数值水平,但可以对养分有效性,植物发育或环境质量产生深远的影响。在大多数情况下,不可能将某种特定生物的数量与其在土壤生态系统中的重要性等同起来。此外,任何种群或活动规模的枚举都代表了一个时间点的测量,该测量处于某种由物理、化学和生物环境控制的动态平衡状态。变异对大多数科学家来说是一个熟悉的问题,尤其是那些处理环境问题或栖息地的科学家。即使是土壤科学家新手也认识到,不同地点的土壤是不同的,这是基于可观察到的差异,如颜色、深度或土壤层的排列。不太明显的事实是,不仅土壤的总体性质因地点而异,而且在一个地点内,也可能发生显著的变化。直觉上,人们可能会怀疑微生物种群因深度而异,表层通常比地下层有更多的生物体和更丰富的类型。Waksman和Starkey(1931)提供的资料支持这一论点。对于不同的土壤,表层的生物总是比地下的多。这些差异是由于不同土层的物理和化学性质不同,从而导致微生物的异质性分布。除了剖面内的差异外,采样区域内土壤微生物特性的空间差异较小是合理的
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引用次数: 12
Equilibrium Modeling in Soil Chemistry 土壤化学中的平衡模型
Pub Date : 2018-09-11 DOI: 10.2136/SSSABOOKSER5.3.C44
S. Mattigod, J. Zachara
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引用次数: 1
Atomic Absorption and Flame Emission Spectrometry 原子吸收与火焰发射光谱法
Pub Date : 2018-09-11 DOI: 10.2136/SSSABOOKSER5.3.C4
Rosalind J Wright, T. Stuczynski
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引用次数: 58
6.3 Solute Transport: Theoretical Background 6.3溶质迁移:理论背景
Pub Date : 2018-09-11 DOI: 10.2136/SSSABOOKSER5.4.C56
T. Skaggs, F. Leij
The transport of solutes in soils has always been of interest in agronomy because of the impact that nutrient and salt concentrations have on conditions for plant growth. During the last few decades, interest in solute transport has broadened due to concerns about the fate of chemicals in the subsurface environment, particularly with regard to the possible contamination of soil and groundwater by agricultural and industrial chemicals. Although significant progress has been made, the quantitative description of solute transport in soils remains a challenging and active area of research. In this section we review basic theoretical concepts and models for solute transport in soils (miscible displacement). Later sections discuss experimental procedures (Section 6.4) and methods of data analysis (Section 6.5).
由于养分和盐浓度对植物生长条件的影响,土壤中溶质的运输一直是农学研究的热点。在过去几十年里,由于对化学品在地下环境中的命运的关注,特别是对农业和工业化学品可能污染土壤和地下水的关注,对溶质运输的兴趣已经扩大。尽管已经取得了重大进展,但土壤中溶质迁移的定量描述仍然是一个具有挑战性和活跃的研究领域。在本节中,我们回顾了溶质在土壤中运移(混相位移)的基本理论概念和模型。后面的章节讨论实验程序(第6.4节)和数据分析方法(第6.5节)。
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引用次数: 5
Testing Soils for Copper, Iron, Manganese, and Zinc 铜、铁、锰和锌的土壤试验
Pub Date : 2018-09-11 DOI: 10.2136/SSSABOOKSER3.3ED.C9
W. Lindsay, D. C. Martens
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引用次数: 53
Water Retention: Field Methods 水保持:现场方法
Pub Date : 2018-09-11 DOI: 10.2136/SSSABOOKSER5.1.2ED.C27
R. R. Bruce, R. Luxmoore
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引用次数: 24
1.8 Newer Application Techniques 1.8更新的应用技术
Pub Date : 2018-09-11 DOI: 10.2136/SSSABOOKSER5.4.C8
A. McBratney, A. Anderson, R. M. Lark, I. Odeh
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引用次数: 0
Hydraulic Conductivity, Diffusivity, and Sorptivity of Unsaturated Soils: Field Methods 非饱和土壤的水力导电性、扩散性和吸附性:现场方法
Pub Date : 2018-09-11 DOI: 10.2136/SSSABOOKSER5.1.2ED.C30
R. Green, L. Ahuja, S. Chong
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引用次数: 80
6.4 Solute Transport: Experimental Methods 6.4溶质迁移:实验方法
Pub Date : 2018-09-11 DOI: 10.2136/SSSABOOKSER5.4.C57
T. Skaggs, Glenn V. Wilson, P. Shouse, F. Leij
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引用次数: 4
Aluminum Hydroxides and Oxyhydroxides 氢氧化铝和氢氧化物
Pub Date : 2018-09-11 DOI: 10.2136/SSSABOOKSER1.2ED.C7
P. Hsu
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引用次数: 45
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