木质植物的侵蚀改变了碳酸盐基岩:现场证据表明,气候变化和透性得到了增强
Pedro A M Leite1, Logan M Schmidt2,3, Daniella M Rempe2
1Department of Ecology and Conservation Biology, Texas A&M University, College Station, TX, USA. pedroleite@tamu.edu.
Scientific reports
|September 18, 2023
概括
木质植物的侵占显著增加了基岩的透性,通过增强石灰岩的气候和多孔性. 这一过程被观察了80多年,深化了植物根和岩石多孔性,影响了生态水文学.
科学领域:
- 生态水文学 生态水文学
- 地质地质地质地质地质地
- 生物地质化学生物地质化学
背景情况:
- 木质植物侵占是一个普遍的现象,对基石水力性能的影响不太了解.
- 以前的研究表明,由于木质植物的侵占,石灰岩的气候变化加速.
研究的目的:
- 评估木质植物侵蚀加速石灰岩气候变化并改变基石水力特性的假设.
- 量化木质植物侵蚀对基岩透性及其相关因素的影响.
主要方法:
- 德克萨斯州爱德华兹高原的实地研究,比较侵占和非侵占的基石地点.
- 在现场进行穿透性测试,使用经过气候变化的岩基中的钻孔.
- 分析了 regolith 厚度,植物植根深度,岩石硬度和石灰岩矩阵多孔性.
主要成果:
- 基岩的平均和液压导电性在木质植物下是一个数量级的高.
- 侵占导致了高质层厚度的增加和植物根深度的增加.
- 观察到岩石硬度显著下降,石灰岩基质多孔度增加了24-44%.
结论:
- 木质植物的侵占增强了基岩的气候变化,显著增加了透性.
- 这创造了一个积极的反循环,可能会在几十年内造成实质性的景观变化.
- 需要进一步研究对气候变化率和透性的更广泛影响.
更多相关视频
07:22Author Spotlight: Unraveling the Role of Earthworms in Enhancing Mineral Weathering for CO2 Removal
Published on: November 10, 2023
3.5K
08:09Measuring and Mapping Patterns of Soil Erosion and Deposition Related to Soil Carbonate Concentrations Under Agricultural Management
Published on: September 12, 2017
11.8K
相关概念视频
Carbonation Shrinkage
165
Atmospheric CO2 penetrates the concrete's pores and, in the presence of moisture, forms carbonic acid, which then reacts with calcium hydroxide in the hydrated cement, forming calcium carbonate. This process reduces the concrete's volume and is termed carbonation shrinkage.
The concrete's permeability is slightly reduced as calcium carbonate produced during the reaction fills its pores. Furthermore, its strength is slightly enhanced as the water released during the reaction...
The concrete's permeability is slightly reduced as calcium carbonate produced during the reaction fills its pores. Furthermore, its strength is slightly enhanced as the water released during the reaction...
165
Permeability of Concrete
171
Permeability in the context of concrete refers to how easily liquids or gases can pass through the material. This quality is crucial for assessing the water-tightness and durability of concrete structures and their resistance to chemical attacks. Concrete permeability can be determined through comparative laboratory tests. These tests typically involve sealing a concrete specimen from the sides, applying water pressure to the top surface with pressure, and measuring the amount of water passing...
171
Porosity and Absorption of Aggregate
317
Aggregates contain pores of varying sizes; while some are completely enclosed within the particles, others open onto the surface, allowing water to penetrate. The porosity of aggregates is a major factor contributing to the overall porosity of concrete, given that aggregates constitute about three-quarters of concrete's volume.
When all pores in an aggregate are filled with water, the aggregate is considered saturated and surface-dry. If left in dry air, water will evaporate until the...
When all pores in an aggregate are filled with water, the aggregate is considered saturated and surface-dry. If left in dry air, water will evaporate until the...
317
Porosity in Cement Paste
170
The porosity of concrete is a measure of the void spaces within its structure. These spaces impact its strength and durability significantly. When water and cement interact, a chemical reaction called hydration creates a semi-solid paste. This paste includes combined water, making up approximately 23% of the cement's dry mass, and gel water, which fills minuscule voids known as gel pores, accounting for about 28% of the cement gel volume.
The balance of water to cement in the mix is...
The balance of water to cement in the mix is...
170
Effect of Sea Water on Concrete
278
Concrete exposed to seawater can undergo degradation like the dissolution of ettringite and gypsum, increasing the material's porosity and decreasing its strength. In contrast, the crystallization of salts within the concrete's pores can cause expansion, particularly above the waterline where evaporation occurs. Nonetheless, this expansion only happens when seawater, enabled by the concrete's permeability, manages to infiltrate the structure.
Concrete in areas between tide marks,...
Concrete in areas between tide marks,...
278
Habitat Fragmentation
17.6K
Habitat fragmentation describes the division of a more extensive, continuous habitat into smaller, discontinuous areas. Human activities such as land conversion, as well as slower geological processes leading to changes in the physical environment, are the two leading causes of habitat fragmentation. The fragmentation process typically follows the same steps: perforation, dissection, fragmentation, shrinkage, and attrition.
17.6K
