Results 41 to 50 of about 1,183 (154)

Controlling influence of the “perched water structure” on rainfall-induced landslide: A case study of the Yaogou landslide in Zhushan County, Hubei Province [PDF]

open access: yes
The Yaogou landslide, located in Zhushan County, Hubei Province, exhibits distinctive aquifer characteristics and varying permeability, leading to the retention of groundwater within the landslide after rainfall, forming confined water.
Lihua LI   +3 more
core   +1 more source

初始含水率对崩岗土体抗拉特性的影响

open access: yesShuitu Baochi Xuebao, 2019
针对花岗岩发育的崩岗土体崩壁失稳等问题,通过单轴抗拉试验,研究了湖北通城地区不同初始含水率的崩岗土体抗拉强度特性。结果表明:初始含水率对崩岗土壤抗拉强度影响明显。土壤抗拉强度特征曲线为单峰型,表土层、红土层和红砂过渡层抗拉特征曲线在含水率WC(24.4%)附近出现抗拉强度峰值,而砂土层在WC(25.8%)出现抗拉强度峰值。崩岗不同层次土壤轴向拉伸长和径向收缩长随初始含水率呈现正相关关系,且土壤轴向拉伸率和径向收缩率与初始含水率拟合出相关系数较高的线性函数关系 ...
冯延云   +3 more
doaj  

含岩屑紫色土水分扩散规律

open access: yesShuitu Baochi Xuebao, 2020
紫色土中存在的岩屑显著影响土壤水分扩散。以往研究主要集中在 > 2 mm岩屑上而忽视了 < 2 mm岩屑的作用。因此,探讨 > 2 mm岩屑对紫色土水分扩散的影响基础上,明确 < 2 mm岩屑的作用对完善含岩屑紫色土水分扩散规律的研究具有重要的意义,从而为土壤水动力学模型的构建提供理论依据。以四川盆地紫色页岩发育的暗棕紫泥土和泥岩发育的红棕紫泥土为研究对象,设置3种岩屑粒径(0.25~2,2~5,5~10 mm)和4种岩屑含量(0,30%,50%,70%),利用水平土柱吸渗法测定含岩屑土壤湿润锋变化特征、
李江文   +4 more
doaj  

Driving factors analysis of surface soil moisture variation in Zhangjiakou-Chengde district based on geodetector [PDF]

open access: yes
As an important water conservation and sand-windy barrier, Zhangjiakou and Chengde (Zhang-Cheng) district of Hebei Province is very important for ecological protection in the Beijing-Tianjin-Hebei region.
Aifang JIN   +4 more
core   +1 more source

土壤初始含水率对涌泉根灌土壤水分及氮素运移特性的影响

open access: yesShuitu Baochi Xuebao, 2017
为了探究涌泉根灌水肥一体化灌溉在不同土壤初始含水率下水氮运移特性,通过室内肥液入渗试验,研究了不同土壤初始含水率(4.13%,7.21%,8.77%,11.06%,14.01%)条件下累积入渗量的入渗特性、湿润锋运移、土壤水分以及铵态氮和硝态氮的运移特性,建立了涌泉根灌累积入渗量、各向湿润锋运移距离与不同土壤初始含水率之间的关系,提出了不同初始含水率下涌泉根灌累积入渗量、各向湿润锋运移距离的经验模型。结果表明:累积入渗量、各向湿润锋运移距离以及湿润体内水分和氮素的分布 ...
刘 显   +5 more
doaj  

太湖地区主要水稻土的土壤水分参数研究

open access: yesShuitu Baochi Xuebao, 2001
太湖地区主要水稻土类型的水分参数研究结果表明 ,水稻土 4个土层的土壤水分特征曲线基本一致。土壤的饱和含水量、田间持水量、凋萎系数和土壤有效水的含量均从土壤上层到下层呈降低的趋势 ;土壤的非饱和导水率与负压水头之间呈负相关的指数曲线变化 ,当负压水头达到 10 k Pa时 ,非饱和导水率降低到最小值 ,且基本趋于稳定 ;非饱和土壤水扩散率变化于 1.1× 10 - 3~ 1.886× 10 - 3cm2 / min之间 ,非饱和土壤水扩散率随含水量也呈指数曲线变化。
陈效民 潘根兴 沈其荣 王德建
doaj  

Greenhouse Gas Mitigation and Yield Response to Biochar-Microbial Amendment in Saline-Alkali Soil [PDF]

open access: yes
[Objective] To investigate the effects of combined application of biochar and microbial fertilizer on greenhouse gas emissions and sunflower yield in saline-alkali soil under plastic film mulching and drip irrigation.
JI Wentao   +6 more
core   +1 more source

土壤初始含水率对浑水膜孔灌自由入渗特性影响

open access: yesShuitu Baochi Xuebao, 2016
为揭示土壤初始含水率对浑水膜孔灌单点源自由入渗的影响,通过开展不同初始含水率的室内浑水膜孔灌试验,研究了土壤初始含水率对浑水膜孔灌自由入渗特性、减渗特性以及土壤含水率分布的影响,并建立了基于土壤初始含水率和累积入渗时间的浑水膜孔灌自由入渗模型和减渗模型。研究表明:当浑水的含沙率和膜孔的直径一定时,随土壤初始含水率的增大,相同时间内的单位膜孔面积累积入渗量呈逐渐减小的趋势,初始含水率为4.96%,7.43%,10.07%和12.40%的分别较风干条件下的减少了19%,33%,45%和56%,减渗效果明显 ...
金世杰   +5 more
doaj  

Effect of Freezing on Wind Erosion Resistance of Sand Dune Soil [PDF]

open access: yes
[Objective] To investigate the effect of winter soil freezing on soil erodibility and anti-erodibility in the Yellow River section of the Ulan Buh Desert.
DOU Chunhua   +4 more
core   +1 more source

咸水结冰灌溉下盐碱地土壤水热盐动态迁移特征分析

open access: yesShuitu Baochi Xuebao, 2023
为探究合理的咸水结冰灌溉水量及咸水结冰灌溉下冻融期土壤水热盐动态迁移规律,以重度盐碱地为研究对象,在内蒙古达拉特旗开展连续2年田间小区原位冻融试验,设置4组灌水梯度,灌水量分别为140 mm (S1),180 mm (S2),220 mm (S3)以及不进行灌溉对照(CK),灌溉水矿化度为8~10 g/L。通过测定试验期内土壤含水率、土壤温度以及盐分分布,分析咸水结冰灌溉下盐碱地土壤水热盐动态迁移特征。结果表明:咸水结冰灌溉可显著提高春季消融后土壤含水率,减缓冻融期深层土壤温度变异程度 ...
李俊杰   +4 more
doaj  

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