[PDF][PDF] Geomorphology and natural hazards in karst areas: a review
Since human beings started to colonise the world, slowly migrating (in multiple directions)
from the African Rift and ultimately reaching the southernmost territories of the Americas …
from the African Rift and ultimately reaching the southernmost territories of the Americas …
[HTML][HTML] 塔北哈拉哈塘奥陶系碳酸盐岩岩溶储层发育特征及主要岩溶期次
张学丰， 李明， 陈志勇， 姜华， 唐俊伟， 刘波， 高计县… - 岩石学报, 2012 - html.rhhz.net
位于塔北隆起中部的哈拉哈塘地区, 具有良好的油气成藏条件, 是近期塔北油气勘探的突破新区,
勘探的主要目标是奥陶系碳酸盐岩岩溶储层. 本文通过对区域沉积, 构造演化背景的分析 …
勘探的主要目标是奥陶系碳酸盐岩岩溶储层. 本文通过对区域沉积, 构造演化背景的分析 …
Influence of diel biogeochemical cycles on carbonate equilibrium in a karst river
Variations in temperature, photosynthesis, and respiration force diel variations in pH and
dissolved CO2 concentrations of surface streams, possibly controlling carbonate equilibrium …
dissolved CO2 concentrations of surface streams, possibly controlling carbonate equilibrium …
Water exchange and pressure transfer between conduits and matrix and their influence on hydrodynamics of two karst aquifers with sinking streams
Karst aquifers are heterogeneous media where conduits usually drain water from lower
permeability volumes (matrix and fractures). For more than a century, various approaches …
permeability volumes (matrix and fractures). For more than a century, various approaches …
Application of MODFLOW for simulating groundwater flow in the Trifilia karst aquifer, Greece
G Panagopoulos - Environmental Earth Sciences, 2012 - Springer
Karst aquifers can have a complex flow as a result of the formation of large conduits from
dissolution features. As a result, a three-dimensional finite-difference groundwater flow …
dissolution features. As a result, a three-dimensional finite-difference groundwater flow …
Characterization of groundwater and surface water mixing in a semiconfined karst aquifer using time‐lapse electrical resistivity tomography
SB Meyerhoff, RM Maxwell, A Revil… - Water Resources …, 2014 - Wiley Online Library
Groundwater flow in karst includes exchange of water between large fractures, conduits, and
the surrounding porous matrix, which impacts both water quality and quantity. Electrical …
the surrounding porous matrix, which impacts both water quality and quantity. Electrical …
Groundwater‐surface water interaction, dissolved organic carbon oxidation and dissolution in carbonate aquifers
A Oberhelman, JB Martin… - Earth Surface Processes …, 2024 - Wiley Online Library
The high primary porosity and permeability of eogenetic karst aquifers permit water
recharged through secondary dissolution features to be temporarily stored in aquifer matrix …
recharged through secondary dissolution features to be temporarily stored in aquifer matrix …
Formation of phreatic caves in an eogenetic karst aquifer by CO2 enrichment at lower water tables and subsequent flooding by sea level rise
Formation of extensive phreatic caves in eogenetic karst aquifers is widely believed to
require mixing of fresh and saltwater. Extensive phreatic caves also occur, however, in …
require mixing of fresh and saltwater. Extensive phreatic caves also occur, however, in …
River reversals into karst springs: A model for cave enlargement in eogenetic karst aquifers
Most conceptual models of epigenic conduit development assume that conduits sourcing
karst springs form as water that is undersaturated with respect to carbonate minerals flows …
karst springs form as water that is undersaturated with respect to carbonate minerals flows …
Groundwater recharge in semi-arid karst context using chloride and stable water isotopes
The karst aquifers of India are an indispensable source of water to millions of people but the
current globalization and climate change have altered the hydrological and other processes …
current globalization and climate change have altered the hydrological and other processes …