Results 21 to 30 of about 1,460,352 (153)

古尔班通古特沙漠腹地土壤水分时空分异研究

open access: yesShuitu Baochi Xuebao, 2004
古尔班通古特沙漠土壤水分补给以积雪融水和雨水为主,土壤水分是维系古尔班通古特沙漠荒漠植被发育最主要的制约因子。选取沙漠腹地典型沙垄为研究区,并分地貌部位布设了土壤水分监测点、植物监测样方以及沙面蚀积监测铁钎和气象观测站,从而形成以土壤水分监测为主的综合监测场。通过野外标定,利用中子水分仪对典型沙垄的不同地貌部位土壤水分动态进行系统监测,结果表明:土壤水分受季节性积雪、降雨、地貌部位、地形起伏、植被盖度等因素的影响而出现明显的空间分异与时间变化。土壤水分的空间差异整体表现为垄问土壤水分高于垄顶 ...
赵从举 康慕谊 雷加强
doaj   +2 more sources

Farm‐Scale Recharge Pits for Improving Local Groundwater Availability: Insights From a Hardrock Watershed in Rajasthan, India

open access: yesWorld Water Policy, Volume 12, Issue 3, August 2026.
ABSTRACT Groundwater depletion is a major challenge in semiarid, hard‐rock regions where irrigation demands often exceed natural recharge. This study evaluates the effectiveness of farm‐scale recharge pits as a local, supplementary, and community‐managed groundwater recharge solution in the Dharta catchment of Rajasthan, India. Alongside check dams and
Prahlad Soni   +4 more
wiley   +1 more source

Alleviation of phosphorus rather than nitrogen limitation driven by permafrost and landscape effects on Dahurian larch forests

open access: yesFunctional Ecology, Volume 40, Issue 8, Page 2590-2601, August 2026.
Read the free Plain Language Summary for this article on the Journal blog. Abstract Permafrost thaw is reshaping nutrient dynamics in boreal forests, but its impacts on tree nutrient limitation and functional strategies remain poorly understood. Clarifying these responses is crucial for predicting the response of boreal forests to climate change.
Qiyue Fu   +9 more
wiley   +1 more source

Land use overrides climatic controls on soil organic nitrogen transformations: Contrasting responsiveness between forest and cropland ecosystems

open access: yesFunctional Ecology, Volume 40, Issue 7, Page 2128-2142, July 2026.
Read the free Plain Language Summary for this article on the Journal blog. Abstract Soil organic nitrogen (SON) transformation is critical for global nutrient cycling and ecosystem productivity, yet how its responsiveness to climate change differs across diverse land use types remains poorly resolved.
Xinyi Yang   +10 more
wiley   +1 more source

Developmental plasticity drives converge nt shifts in phosphorus acquisition strategies towards root phosphatase activity in Moso bamboo under nitrogen addition

open access: yesFunctional Ecology, Volume 40, Issue 7, Page 2221-2236, July 2026.
Read the free Plain Language Summary for this article on the Journal blog. Abstract Anthropogenic nitrogen (N) deposition is a major driver of global change. However, its effects on the developmental plasticity of plant nutrient strategies remain poorly understood.
Quan Li   +11 more
wiley   +1 more source

季节性干旱区紫色土坡耕地土壤水分对降雨的响应

open access: yesShuitu Baochi Xuebao, 2020
以金沙江下游季节性干旱区紫色土坡耕地为研究对象,使用PR2/6土壤剖面水分测定仪和翻斗式雨量计对雨季0—100 cm土层的土壤含水量和降雨量进行连续观测,分析雨季紫色土土壤水分对降雨的响应。结果表明:每月平均土壤含水量之间存在显著差异,0—20 cm土壤含水率表现为9月 > 8月≈7月 > 6月,在整个雨季呈累加上升趋势。降雨量大小是影响土壤水分补给深度的决定因素。小雨(6.4 mm)只对10 cm土层土壤水分产生影响,平均提高12.35%;中雨(23 mm)对30 cm以上土层土壤水分产生影响,10 ...
徐露   +5 more
doaj  

石羊河中游荒漠绿洲区土壤水分的分布特征

open access: yesShuitu Baochi Xuebao, 2007
通过田间实验,研究了不同土壤层颗粒组成、土壤水分的分布特征及不同土壤层间土壤水分的关联性。结果表明:(1)土壤颗粒组成决定了不同土壤层的持水性能,是导致土壤水的分布及运动方式发生变化,影响水分在土壤中滞留时间的根本原因,土壤层中的砂砾所占百分数越大,粘粒含量就越少,含水率就越小,壤土中的土壤水分滞留时间远大于砂质土壤。(2)试验区3m内土壤层可分为水分散失带、水分滞留带和水分过渡带,水分滞留带是土壤水分暂时贮存的重要土层,也是为植被提供深层土壤水分的直接来源,对植被的生长及农作物生产有重要的影响 ...
李王成   +4 more
doaj  

中国西南水梯田土壤水分特性研究——以哈尼梯田为例

open access: yesShuitu Baochi Xuebao, 2021
为了研究中国西南水梯田的土壤水分特性,以云南哈尼梯田为例,选取哈尼梯田核心区全福庄小流域内林地、荒草地、旱地和水田4种土地利用类型,分层取0—10,10—20,20—40,40—60,60—80,80—100 cm深度土样测其主要土壤理化指标和土壤水分特征曲线,分析其土壤的持水性和水分有效性。结果表明:(1)哈尼梯田4种不同土地利用类型土壤容重变化范围为0.61~1.41 g/cm3,且0—40 cm与40—100 cm差异性显著,土壤有机质含量为1.17%~9.65 ...
李源, 宋维峰, 马建刚
doaj  

The underappreciated roles of fog and dew on vegetation and biocrusts

open access: yesNew Phytologist, Volume 251, Issue 1, Page 46-63, July 2026.
Summary Fog and dew represent minor components of ecosystem water budgets in most ecosystems. However, fog and dew can play an essential role in ecosystem dynamics and are particularly important for water‐limited systems. In addition to serving as direct water inputs, fog and dew can influence microclimate and water redistribution, thereby promoting ...
Lixin Wang, Yue Li, Mengyun Sun, Na Qiao
wiley   +1 more source

丹江口库区石渣土土壤水分有效性研究

open access: yesShuitu Baochi Xuebao, 2002
土壤水分有效性的高低是制约石渣土生产能力的关键因素之一。对丹江口库区郧县石渣土 3种不同土石比土壤水分有效性的研究表明 :土壤水分有效性与土壤中的土 (2 mm)比关系密切。土壤蒸发、持水、导水和供水能力均与土壤中的土石比的大小有关。 3种土壤的持水能力 ,以石砾含量较少、质地较粘的土壤最强 ,以石砾含量较多、质地为壤质的土壤最低。而土壤水分蒸发能力与砾石含量呈负相关 ,土壤水分扩散率则与砾石含量呈正相关。适中土石比的土壤可提高入渗性能 ,减少蒸发量 ,提高供水性能。
吕国安 蔡崇法 等
doaj   +2 more sources

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