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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
2.5 Specific Surface Area 2.5比表面积
Pub Date : 2018-09-11 DOI: 10.2136/SSSABOOKSER5.4.C13
K. Pennell
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引用次数: 12
3.3.3 Field 3.3.3领域
Pub Date : 2018-09-11 DOI: 10.2136/SSSABOOKSER5.4.C26
N. Romano, A. Santini
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引用次数: 8
3.2.1 Piezometry 3.2.1压力测定
Pub Date : 2018-09-11 DOI: 10.2136/SSSABOOKSER5.4.C20
Michael H. Young
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引用次数: 1
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
3.3.4 Parametric Models 3.3.4参数化模型
Pub Date : 2018-09-11 DOI: 10.2136/SSSABOOKSER5.4.C27
Ken'ichirou Kosugi, Jan W. Hopmans, Jacob H. Dane
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引用次数: 8
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
Plant Analysis as an Aid in Fertilizing Tobacco 植物分析在烟草施肥中的辅助作用
Pub Date : 2018-09-11 DOI: 10.2136/SSSABOOKSER3.3ED.C24
G. Miner, M. Tucker
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引用次数: 7
6.5 Solute Transport: Data Analysis and Parameter Estimation 6.5溶质迁移:数据分析和参数估计
Pub Date : 2018-09-11 DOI: 10.2136/SSSABOOKSER5.4.C58
T. Skaggs, D. Jaynes, R. Kachanoski, P. Shouse, A. Ward
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引用次数: 1
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
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