Results 1 to 10 of about 594 (95)

SWAMP: A new experiment for simulating permafrost warming and active layer deepening on the Tibetan Plateau

open access: yesMethods in Ecology and Evolution, Volume 14, Issue 7, Page 1732-1746, July 2023., 2023
Abstract Our knowledge on the responses of permafrost ecosystems to climate warming is critical for assessing the direction and magnitude of permafrost carbon‐climate feedback. However, most of the previous experiments have only been able to warm the air and surface soil, with limited effects on the permafrost temperature.
Yuxuan Bai   +8 more
wiley   +1 more source

Effects of interactions between anthropogenic stressors and recurring perturbations on ecosystem resilience and collapse

open access: yesConservation Biology, Volume 37, Issue 1, February 2023., 2023
Abstract Insights into declines in ecosystem resilience and their causes and effects can inform preemptive action to avoid ecosystem collapse and loss of biodiversity, ecosystem services, and human well‐being. Empirical studies of ecosystem collapse are rare and hampered by ecosystem complexity, nonlinear and lagged responses, and interactions across ...
David A. Keith   +8 more
wiley   +1 more source

A novel red‐edge spectral index for retrieving the leaf chlorophyll content

open access: yesMethods in Ecology and Evolution, Volume 13, Issue 12, Page 2771-2787, December 2022., 2022
Abstract The leaf chlorophyll content (Chlleaf) is a crucial vegetation parameter in carbon cycle modelling and agricultural monitoring at local, regional and global scales. The red‐edge spectral region is sensitive to variations in Chlleaf. An increasing number of sensors are capable of sampling red‐edge bands, providing opportunities to estimate ...
Hu Zhang   +15 more
wiley   +1 more source

黄土和红壤坡面侵蚀差异及其与土壤性质的关系

open access: yesShuitu Baochi Xuebao, 2023
为探究黄土和红壤侵蚀受雨强和坡度影响的差异及其与土壤性质的关系,通过测定分析黄土和红壤的各种理化性质,并分别对2种土壤在2个坡度(15°,20°)、2个雨强(60,90 mm/h)条件下开展4场降雨。结果表明:(1)与红壤相比,黄土的土壤颗粒更细,二者的毛管孔隙度、饱和含水量和田间持水量相差均在3%~6%以内,干筛时各粒级团聚体相差不大,但经湿筛破坏后二者团聚体差异较大,红壤的相对机械破碎指数(RMI)小于黄土,黄土有机质含量、阳离子交换量和络合态氧化物含量均高于红壤,无定形氧化物和游离氧化物则低于红壤;
金鑫   +6 more
doaj  

桂西北喀斯特区石灰土与红壤坡地幼龄橘园降雨侵蚀特征

open access: yesShuitu Baochi Xuebao, 2023
为探究桂西北喀斯特区石灰土与红壤坡地幼龄橘园的降雨侵蚀特征,通过室内人工模拟降雨试验,研究3种降雨强度(30,60,90 mm/h)下,石灰土与红壤坡地幼龄橘园的产流产沙特征。结果表明:(1)降雨强度为30,60 mm/h时,红壤橘园的产流总量分别为石灰土橘园的2.46,1.83倍,且红壤橘园主要以地表产流为主,石灰土橘园主要以壤中流产流为主;当降雨强度为90 mm/h时,二者产流总量无显著性差异(p>0.05),均以地表产流为主。(2)石灰土橘园与红壤橘园地表径流强度随降雨强度增大而增大 ...
郑金德   +5 more
doaj  

模拟酸雨对红壤结构体及其胶结物影响的实验研究

open access: yesShuitu Baochi Xuebao, 2002
通过模拟酸雨对浙江杭州红壤的淋溶实验 ,研究了酸雨对红壤结构体及其胶结物的影响。结果表明 ,酸雨降低了红壤团聚体的稳定性 ,表现为水稳性大团聚体的含量随酸雨 p H值的降低、持续时间的延长而减少 ;酸雨导致团聚体破坏率增高、稳定性降低。酸雨对红壤胶结物质的影响 ,表现为土壤有机质淋失增加 ,氧化铁活性提高。红壤团聚体的稳定性和结构性变差 ,会加速土壤侵蚀 ,表现出酸雨对红壤的可蚀性。
许中坚 刘广深 等
doaj   +2 more sources

红薯藤及其生物质炭还田对旱地红壤微生物活性及养分含量的影响

open access: yesShuitu Baochi Xuebao, 2022
为探究红薯藤及其生物质炭还田对旱地红壤微生物活性及养分含量的影响, 通过田间定位试验, 设置5个处理: (1)常规处理(CK); (2)3 000 kg/hm2红薯藤还田(S1);(3)6 000 kg/hm2红薯藤还田(S2);(4)1 000 kg/hm2红薯藤生物质炭还田(BC1);(5)2 000 kg/hm2红薯藤生物质炭还田(BC2), 研究不同剂量红薯藤及其生物质炭还田对红壤微生物活性和养分含量的影响。结果表明: 与CK相比, 在0—10 cm土层中, BC1的土壤基础呼吸增加17.93%,
郜茹茹   +6 more
doaj  

Indian Pangolin in Lamjung Requires Urgent Attention 尼泊尔拉姆琼县地区的印度穿山甲急需关注

open access: yesWildlife Letters, Volume 2, Issue 4, Page 204-213, December 2024.
This study documented the first evidence of the Indian pangolin in Lamjung district, Nepal, finding three burrows and rescue evidence in Simalchaur Naringhat Community Forest. The burrows identified at an elevation of 530 m and characterized by moderate crown and ground cover (26%–50%), a 25° slope, and predominantly red soil, are indicative of a ...
Asmit Neupane   +4 more
wiley   +1 more source

不同经营类型红松林对汤旺河流域土壤性质的影响

open access: yesShuitu Baochi Xuebao, 2006
通过实地调查与试验分析,研究了汤旺河流域4种经营类型红松林对土壤性质的影响情况。结果表明:在研究地区无论土壤pH、土壤有机质,还是土壤养分和土壤物理性质,白桦与红松天然更新形成的混变林和白桦与红松人工造林形成的混交林都较红松人工纯林优越,维护林分土壤地力及涵养水分的功能强。而红松人工纯林较原始红松林和两种白桦红松混交林维护地力及涵养水分功能弱。研究结果为汤旺河流域森林恢复与重建提供了科学合理的途径。
王树力
doaj   +2 more sources

不同母质红壤坡面产流产沙特征比较

open access: yesShuitu Baochi Xuebao, 2018
采用人工模拟降雨的方法,研究花岗岩、第四纪红黏土、红砂岩3种母质发育的红壤坡面产流产沙特征差异。结果表明:(1)地表产流方面,3种母质红壤地表产流时间为花岗岩红壤<红砂岩红壤<第四纪红壤,总径流量和场均产流速率均为花岗岩红壤>红砂岩红壤>第四纪红壤,其中45 mm/h条件下花岗岩红壤的地表径流量为红砂岩和第四纪红壤的1.79~2.47倍,场均产流速率为后者的1.58~2.32倍。(2)地表产沙方面,在45 mm/h条件下,场均泥沙浓度为第四纪红壤>花岗岩红壤>红砂岩红壤;135 mm/h条件下 ...
徐铭泽, 杨
doaj  

Home - About - Disclaimer - Privacy