Short-term effects of NaCl and Na

NaCl and Na2SO4 are the key factors affecting nitrogen (N) mineralization in the soil of estuarine wetlands. However, it remains unclear how N mineralization responses to NaCl and Na2SO4. In the present study, samples of topsoil (0–10 cm) and subsoil (10–20 cm) were collected in three marshes, inclu...
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Autor*in:	Yang, Jisong [verfasserIn] Liu, Yue [verfasserIn] Shen, Zhuang [verfasserIn] Yu, Miao [verfasserIn] Yu, Yang [verfasserIn] Wang, Zhikang [verfasserIn] Lv, Zhenbo [verfasserIn] Yu, Junbao [verfasserIn]

Format:	E-Artikel
Sprache:	Englisch

Erschienen:	2020

Schlagwörter:	Nitrogen mineralization Salinity NaCl Na Estuarine marsh

Übergeordnetes Werk:	Enthalten in: Catena - New York, NY [u.a.] : Elsevier, 1973, 196
Übergeordnetes Werk:	volume:196

DOI / URN:	10.1016/j.catena.2020.104828

Katalog-ID:	ELV004910702

Internformat


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520			\|a NaCl and Na2SO4 are the key factors affecting nitrogen (N) mineralization in the soil of estuarine wetlands. However, it remains unclear how N mineralization responses to NaCl and Na2SO4. In the present study, samples of topsoil (0–10 cm) and subsoil (10–20 cm) were collected in three marshes, including a Phragmites australis marsh (Pa-marsh), a Suaeda salsa marsh (Ss-marsh) and a mudflat marsh (Mu-marsh), in the Liaohe River estuary. The soil samples were treated by NaCl and Na2SO4, with a set of salinity levels of 0 %Es, 2 %Es, 5 %Es, 10 %Es, 20 %Es and 100 %Es (%Es, percent of equivalent seawater), respectively. After incubating the soil samples for 2 weeks, the contents of NH4 + N and NO3 − N were measured and the net N mineralization rates (Rmin) were calculated. We found that NH4 + N and NO3 − N accumulations in the soil samples of the three marshes in the NaCl and Na2SO4 treatments. Both NaCl and Na2SO4 significantly affected Rmin for the top soil for Pa-marsh in all salinity treatments, whereas salt-effects for Ss- and Mu-marsh soils were only found at 10 %Es and/or 20 %Es levels in the NaCl treatments. There was an ion-specific effect of NaCl and Na2SO4 on N mineralization. NaCl increased Rmin by 114–164% and 86–139% in the topsoil and subsoil of the three marshes, respectively; Na2SO4 increased Rmin by 234% in the topsoil of Pa-marsh and had no effect on Rmin in the other soils. A salt threshold of 50–60%Es was found for NaCl and Na2SO4 impacting on N mineralization of Pa-marsh soil. Salt type, salinity level, wetland type and soil layer were the main factors impacting the N mineralization. The results suggest that the effect of salt on N mineralization could vary with salt type and soil properties.
650		4	\|a Nitrogen mineralization
650		4	\|a Salinity
650		4	\|a NaCl
650		4	\|a Na
650		4	\|a Estuarine marsh
700	1		\|a Liu, Yue \|e verfasserin \|4 aut
700	1		\|a Shen, Zhuang \|e verfasserin \|4 aut
700	1		\|a Yu, Miao \|e verfasserin \|4 aut
700	1		\|a Yu, Yang \|e verfasserin \|4 aut
700	1		\|a Wang, Zhikang \|e verfasserin \|4 aut
700	1		\|a Lv, Zhenbo \|e verfasserin \|4 aut
700	1		\|a Yu, Junbao \|e verfasserin \|4 aut
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912			\|a GBV_ILN_74
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912			\|a GBV_ILN_224
912			\|a GBV_ILN_370
912			\|a GBV_ILN_602
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912			\|a GBV_ILN_2003
912			\|a GBV_ILN_2004
912			\|a GBV_ILN_2005
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912			\|a GBV_ILN_2015
912			\|a GBV_ILN_2020
912			\|a GBV_ILN_2021
912			\|a GBV_ILN_2025
912			\|a GBV_ILN_2027
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912			\|a GBV_ILN_4313
912			\|a GBV_ILN_4323
912			\|a GBV_ILN_4324
912			\|a GBV_ILN_4326
912			\|a GBV_ILN_4333
912			\|a GBV_ILN_4334
912			\|a GBV_ILN_4335
912			\|a GBV_ILN_4338
912			\|a GBV_ILN_4393
936	b	k	\|a 38.60 \|j Bodenkunde: Allgemeines \|x Geowissenschaften
936	b	k	\|a 38.45 \|j Geomorphologie
951			\|a AR
952			\|d 196

Indexfelder

author_variant	j y jy y l yl z s zs m y my y y yy z w zw z l zl j y jy
matchkey_str	article:00087769:2020----::hrtrefcsf
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publishDate	2020
allfields	10.1016/j.catena.2020.104828 doi (DE-627)ELV004910702 (ELSEVIER)S0341-8162(20)30378-7 DE-627 ger DE-627 rda eng 910 550 DE-600 38.60 bkl 38.45 bkl Yang, Jisong verfasserin aut Short-term effects of NaCl and Na 2020 nicht spezifiziert zzz rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier NaCl and Na2SO4 are the key factors affecting nitrogen (N) mineralization in the soil of estuarine wetlands. However, it remains unclear how N mineralization responses to NaCl and Na2SO4. In the present study, samples of topsoil (0–10 cm) and subsoil (10–20 cm) were collected in three marshes, including a Phragmites australis marsh (Pa-marsh), a Suaeda salsa marsh (Ss-marsh) and a mudflat marsh (Mu-marsh), in the Liaohe River estuary. The soil samples were treated by NaCl and Na2SO4, with a set of salinity levels of 0 %Es, 2 %Es, 5 %Es, 10 %Es, 20 %Es and 100 %Es (%Es, percent of equivalent seawater), respectively. After incubating the soil samples for 2 weeks, the contents of NH4 + N and NO3 − N were measured and the net N mineralization rates (Rmin) were calculated. We found that NH4 + N and NO3 − N accumulations in the soil samples of the three marshes in the NaCl and Na2SO4 treatments. Both NaCl and Na2SO4 significantly affected Rmin for the top soil for Pa-marsh in all salinity treatments, whereas salt-effects for Ss- and Mu-marsh soils were only found at 10 %Es and/or 20 %Es levels in the NaCl treatments. There was an ion-specific effect of NaCl and Na2SO4 on N mineralization. NaCl increased Rmin by 114–164% and 86–139% in the topsoil and subsoil of the three marshes, respectively; Na2SO4 increased Rmin by 234% in the topsoil of Pa-marsh and had no effect on Rmin in the other soils. A salt threshold of 50–60%Es was found for NaCl and Na2SO4 impacting on N mineralization of Pa-marsh soil. Salt type, salinity level, wetland type and soil layer were the main factors impacting the N mineralization. The results suggest that the effect of salt on N mineralization could vary with salt type and soil properties. Nitrogen mineralization Salinity NaCl Na Estuarine marsh Liu, Yue verfasserin aut Shen, Zhuang verfasserin aut Yu, Miao verfasserin aut Yu, Yang verfasserin aut Wang, Zhikang verfasserin aut Lv, Zhenbo verfasserin aut Yu, Junbao verfasserin aut Enthalten in Catena New York, NY [u.a.] : Elsevier, 1973 196 Online-Ressource (DE-627)30272432X (DE-600)1492500-X (DE-576)081952821 0008-7769 nnns volume:196 GBV_USEFLAG_U SYSFLAG_U GBV_ELV SSG-OPC-GGO GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_32 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_74 GBV_ILN_90 GBV_ILN_95 GBV_ILN_100 GBV_ILN_105 GBV_ILN_110 GBV_ILN_150 GBV_ILN_151 GBV_ILN_224 GBV_ILN_370 GBV_ILN_602 GBV_ILN_702 GBV_ILN_2003 GBV_ILN_2004 GBV_ILN_2005 GBV_ILN_2011 GBV_ILN_2014 GBV_ILN_2015 GBV_ILN_2020 GBV_ILN_2021 GBV_ILN_2025 GBV_ILN_2027 GBV_ILN_2034 GBV_ILN_2038 GBV_ILN_2044 GBV_ILN_2048 GBV_ILN_2049 GBV_ILN_2050 GBV_ILN_2056 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 GBV_ILN_2111 GBV_ILN_2112 GBV_ILN_2113 GBV_ILN_2118 GBV_ILN_2122 GBV_ILN_2129 GBV_ILN_2143 GBV_ILN_2147 GBV_ILN_2148 GBV_ILN_2152 GBV_ILN_2153 GBV_ILN_2190 GBV_ILN_2336 GBV_ILN_2507 GBV_ILN_2522 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4242 GBV_ILN_4251 GBV_ILN_4305 GBV_ILN_4313 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4326 GBV_ILN_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4338 GBV_ILN_4393 38.60 Bodenkunde: Allgemeines Geowissenschaften 38.45 Geomorphologie AR 196
spelling	10.1016/j.catena.2020.104828 doi (DE-627)ELV004910702 (ELSEVIER)S0341-8162(20)30378-7 DE-627 ger DE-627 rda eng 910 550 DE-600 38.60 bkl 38.45 bkl Yang, Jisong verfasserin aut Short-term effects of NaCl and Na 2020 nicht spezifiziert zzz rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier NaCl and Na2SO4 are the key factors affecting nitrogen (N) mineralization in the soil of estuarine wetlands. However, it remains unclear how N mineralization responses to NaCl and Na2SO4. In the present study, samples of topsoil (0–10 cm) and subsoil (10–20 cm) were collected in three marshes, including a Phragmites australis marsh (Pa-marsh), a Suaeda salsa marsh (Ss-marsh) and a mudflat marsh (Mu-marsh), in the Liaohe River estuary. The soil samples were treated by NaCl and Na2SO4, with a set of salinity levels of 0 %Es, 2 %Es, 5 %Es, 10 %Es, 20 %Es and 100 %Es (%Es, percent of equivalent seawater), respectively. After incubating the soil samples for 2 weeks, the contents of NH4 + N and NO3 − N were measured and the net N mineralization rates (Rmin) were calculated. We found that NH4 + N and NO3 − N accumulations in the soil samples of the three marshes in the NaCl and Na2SO4 treatments. Both NaCl and Na2SO4 significantly affected Rmin for the top soil for Pa-marsh in all salinity treatments, whereas salt-effects for Ss- and Mu-marsh soils were only found at 10 %Es and/or 20 %Es levels in the NaCl treatments. There was an ion-specific effect of NaCl and Na2SO4 on N mineralization. NaCl increased Rmin by 114–164% and 86–139% in the topsoil and subsoil of the three marshes, respectively; Na2SO4 increased Rmin by 234% in the topsoil of Pa-marsh and had no effect on Rmin in the other soils. A salt threshold of 50–60%Es was found for NaCl and Na2SO4 impacting on N mineralization of Pa-marsh soil. Salt type, salinity level, wetland type and soil layer were the main factors impacting the N mineralization. The results suggest that the effect of salt on N mineralization could vary with salt type and soil properties. Nitrogen mineralization Salinity NaCl Na Estuarine marsh Liu, Yue verfasserin aut Shen, Zhuang verfasserin aut Yu, Miao verfasserin aut Yu, Yang verfasserin aut Wang, Zhikang verfasserin aut Lv, Zhenbo verfasserin aut Yu, Junbao verfasserin aut Enthalten in Catena New York, NY [u.a.] : Elsevier, 1973 196 Online-Ressource (DE-627)30272432X (DE-600)1492500-X (DE-576)081952821 0008-7769 nnns volume:196 GBV_USEFLAG_U SYSFLAG_U GBV_ELV SSG-OPC-GGO GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_32 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_74 GBV_ILN_90 GBV_ILN_95 GBV_ILN_100 GBV_ILN_105 GBV_ILN_110 GBV_ILN_150 GBV_ILN_151 GBV_ILN_224 GBV_ILN_370 GBV_ILN_602 GBV_ILN_702 GBV_ILN_2003 GBV_ILN_2004 GBV_ILN_2005 GBV_ILN_2011 GBV_ILN_2014 GBV_ILN_2015 GBV_ILN_2020 GBV_ILN_2021 GBV_ILN_2025 GBV_ILN_2027 GBV_ILN_2034 GBV_ILN_2038 GBV_ILN_2044 GBV_ILN_2048 GBV_ILN_2049 GBV_ILN_2050 GBV_ILN_2056 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 GBV_ILN_2111 GBV_ILN_2112 GBV_ILN_2113 GBV_ILN_2118 GBV_ILN_2122 GBV_ILN_2129 GBV_ILN_2143 GBV_ILN_2147 GBV_ILN_2148 GBV_ILN_2152 GBV_ILN_2153 GBV_ILN_2190 GBV_ILN_2336 GBV_ILN_2507 GBV_ILN_2522 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4242 GBV_ILN_4251 GBV_ILN_4305 GBV_ILN_4313 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4326 GBV_ILN_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4338 GBV_ILN_4393 38.60 Bodenkunde: Allgemeines Geowissenschaften 38.45 Geomorphologie AR 196
allfields_unstemmed	10.1016/j.catena.2020.104828 doi (DE-627)ELV004910702 (ELSEVIER)S0341-8162(20)30378-7 DE-627 ger DE-627 rda eng 910 550 DE-600 38.60 bkl 38.45 bkl Yang, Jisong verfasserin aut Short-term effects of NaCl and Na 2020 nicht spezifiziert zzz rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier NaCl and Na2SO4 are the key factors affecting nitrogen (N) mineralization in the soil of estuarine wetlands. However, it remains unclear how N mineralization responses to NaCl and Na2SO4. In the present study, samples of topsoil (0–10 cm) and subsoil (10–20 cm) were collected in three marshes, including a Phragmites australis marsh (Pa-marsh), a Suaeda salsa marsh (Ss-marsh) and a mudflat marsh (Mu-marsh), in the Liaohe River estuary. The soil samples were treated by NaCl and Na2SO4, with a set of salinity levels of 0 %Es, 2 %Es, 5 %Es, 10 %Es, 20 %Es and 100 %Es (%Es, percent of equivalent seawater), respectively. After incubating the soil samples for 2 weeks, the contents of NH4 + N and NO3 − N were measured and the net N mineralization rates (Rmin) were calculated. We found that NH4 + N and NO3 − N accumulations in the soil samples of the three marshes in the NaCl and Na2SO4 treatments. Both NaCl and Na2SO4 significantly affected Rmin for the top soil for Pa-marsh in all salinity treatments, whereas salt-effects for Ss- and Mu-marsh soils were only found at 10 %Es and/or 20 %Es levels in the NaCl treatments. There was an ion-specific effect of NaCl and Na2SO4 on N mineralization. NaCl increased Rmin by 114–164% and 86–139% in the topsoil and subsoil of the three marshes, respectively; Na2SO4 increased Rmin by 234% in the topsoil of Pa-marsh and had no effect on Rmin in the other soils. A salt threshold of 50–60%Es was found for NaCl and Na2SO4 impacting on N mineralization of Pa-marsh soil. Salt type, salinity level, wetland type and soil layer were the main factors impacting the N mineralization. The results suggest that the effect of salt on N mineralization could vary with salt type and soil properties. Nitrogen mineralization Salinity NaCl Na Estuarine marsh Liu, Yue verfasserin aut Shen, Zhuang verfasserin aut Yu, Miao verfasserin aut Yu, Yang verfasserin aut Wang, Zhikang verfasserin aut Lv, Zhenbo verfasserin aut Yu, Junbao verfasserin aut Enthalten in Catena New York, NY [u.a.] : Elsevier, 1973 196 Online-Ressource (DE-627)30272432X (DE-600)1492500-X (DE-576)081952821 0008-7769 nnns volume:196 GBV_USEFLAG_U SYSFLAG_U GBV_ELV SSG-OPC-GGO GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_32 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_74 GBV_ILN_90 GBV_ILN_95 GBV_ILN_100 GBV_ILN_105 GBV_ILN_110 GBV_ILN_150 GBV_ILN_151 GBV_ILN_224 GBV_ILN_370 GBV_ILN_602 GBV_ILN_702 GBV_ILN_2003 GBV_ILN_2004 GBV_ILN_2005 GBV_ILN_2011 GBV_ILN_2014 GBV_ILN_2015 GBV_ILN_2020 GBV_ILN_2021 GBV_ILN_2025 GBV_ILN_2027 GBV_ILN_2034 GBV_ILN_2038 GBV_ILN_2044 GBV_ILN_2048 GBV_ILN_2049 GBV_ILN_2050 GBV_ILN_2056 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 GBV_ILN_2111 GBV_ILN_2112 GBV_ILN_2113 GBV_ILN_2118 GBV_ILN_2122 GBV_ILN_2129 GBV_ILN_2143 GBV_ILN_2147 GBV_ILN_2148 GBV_ILN_2152 GBV_ILN_2153 GBV_ILN_2190 GBV_ILN_2336 GBV_ILN_2507 GBV_ILN_2522 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4242 GBV_ILN_4251 GBV_ILN_4305 GBV_ILN_4313 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4326 GBV_ILN_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4338 GBV_ILN_4393 38.60 Bodenkunde: Allgemeines Geowissenschaften 38.45 Geomorphologie AR 196
allfieldsGer	10.1016/j.catena.2020.104828 doi (DE-627)ELV004910702 (ELSEVIER)S0341-8162(20)30378-7 DE-627 ger DE-627 rda eng 910 550 DE-600 38.60 bkl 38.45 bkl Yang, Jisong verfasserin aut Short-term effects of NaCl and Na 2020 nicht spezifiziert zzz rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier NaCl and Na2SO4 are the key factors affecting nitrogen (N) mineralization in the soil of estuarine wetlands. However, it remains unclear how N mineralization responses to NaCl and Na2SO4. In the present study, samples of topsoil (0–10 cm) and subsoil (10–20 cm) were collected in three marshes, including a Phragmites australis marsh (Pa-marsh), a Suaeda salsa marsh (Ss-marsh) and a mudflat marsh (Mu-marsh), in the Liaohe River estuary. The soil samples were treated by NaCl and Na2SO4, with a set of salinity levels of 0 %Es, 2 %Es, 5 %Es, 10 %Es, 20 %Es and 100 %Es (%Es, percent of equivalent seawater), respectively. After incubating the soil samples for 2 weeks, the contents of NH4 + N and NO3 − N were measured and the net N mineralization rates (Rmin) were calculated. We found that NH4 + N and NO3 − N accumulations in the soil samples of the three marshes in the NaCl and Na2SO4 treatments. Both NaCl and Na2SO4 significantly affected Rmin for the top soil for Pa-marsh in all salinity treatments, whereas salt-effects for Ss- and Mu-marsh soils were only found at 10 %Es and/or 20 %Es levels in the NaCl treatments. There was an ion-specific effect of NaCl and Na2SO4 on N mineralization. NaCl increased Rmin by 114–164% and 86–139% in the topsoil and subsoil of the three marshes, respectively; Na2SO4 increased Rmin by 234% in the topsoil of Pa-marsh and had no effect on Rmin in the other soils. A salt threshold of 50–60%Es was found for NaCl and Na2SO4 impacting on N mineralization of Pa-marsh soil. Salt type, salinity level, wetland type and soil layer were the main factors impacting the N mineralization. The results suggest that the effect of salt on N mineralization could vary with salt type and soil properties. Nitrogen mineralization Salinity NaCl Na Estuarine marsh Liu, Yue verfasserin aut Shen, Zhuang verfasserin aut Yu, Miao verfasserin aut Yu, Yang verfasserin aut Wang, Zhikang verfasserin aut Lv, Zhenbo verfasserin aut Yu, Junbao verfasserin aut Enthalten in Catena New York, NY [u.a.] : Elsevier, 1973 196 Online-Ressource (DE-627)30272432X (DE-600)1492500-X (DE-576)081952821 0008-7769 nnns volume:196 GBV_USEFLAG_U SYSFLAG_U GBV_ELV SSG-OPC-GGO GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_32 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_74 GBV_ILN_90 GBV_ILN_95 GBV_ILN_100 GBV_ILN_105 GBV_ILN_110 GBV_ILN_150 GBV_ILN_151 GBV_ILN_224 GBV_ILN_370 GBV_ILN_602 GBV_ILN_702 GBV_ILN_2003 GBV_ILN_2004 GBV_ILN_2005 GBV_ILN_2011 GBV_ILN_2014 GBV_ILN_2015 GBV_ILN_2020 GBV_ILN_2021 GBV_ILN_2025 GBV_ILN_2027 GBV_ILN_2034 GBV_ILN_2038 GBV_ILN_2044 GBV_ILN_2048 GBV_ILN_2049 GBV_ILN_2050 GBV_ILN_2056 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 GBV_ILN_2111 GBV_ILN_2112 GBV_ILN_2113 GBV_ILN_2118 GBV_ILN_2122 GBV_ILN_2129 GBV_ILN_2143 GBV_ILN_2147 GBV_ILN_2148 GBV_ILN_2152 GBV_ILN_2153 GBV_ILN_2190 GBV_ILN_2336 GBV_ILN_2507 GBV_ILN_2522 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4242 GBV_ILN_4251 GBV_ILN_4305 GBV_ILN_4313 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4326 GBV_ILN_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4338 GBV_ILN_4393 38.60 Bodenkunde: Allgemeines Geowissenschaften 38.45 Geomorphologie AR 196
allfieldsSound	10.1016/j.catena.2020.104828 doi (DE-627)ELV004910702 (ELSEVIER)S0341-8162(20)30378-7 DE-627 ger DE-627 rda eng 910 550 DE-600 38.60 bkl 38.45 bkl Yang, Jisong verfasserin aut Short-term effects of NaCl and Na 2020 nicht spezifiziert zzz rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier NaCl and Na2SO4 are the key factors affecting nitrogen (N) mineralization in the soil of estuarine wetlands. However, it remains unclear how N mineralization responses to NaCl and Na2SO4. In the present study, samples of topsoil (0–10 cm) and subsoil (10–20 cm) were collected in three marshes, including a Phragmites australis marsh (Pa-marsh), a Suaeda salsa marsh (Ss-marsh) and a mudflat marsh (Mu-marsh), in the Liaohe River estuary. The soil samples were treated by NaCl and Na2SO4, with a set of salinity levels of 0 %Es, 2 %Es, 5 %Es, 10 %Es, 20 %Es and 100 %Es (%Es, percent of equivalent seawater), respectively. After incubating the soil samples for 2 weeks, the contents of NH4 + N and NO3 − N were measured and the net N mineralization rates (Rmin) were calculated. We found that NH4 + N and NO3 − N accumulations in the soil samples of the three marshes in the NaCl and Na2SO4 treatments. Both NaCl and Na2SO4 significantly affected Rmin for the top soil for Pa-marsh in all salinity treatments, whereas salt-effects for Ss- and Mu-marsh soils were only found at 10 %Es and/or 20 %Es levels in the NaCl treatments. There was an ion-specific effect of NaCl and Na2SO4 on N mineralization. NaCl increased Rmin by 114–164% and 86–139% in the topsoil and subsoil of the three marshes, respectively; Na2SO4 increased Rmin by 234% in the topsoil of Pa-marsh and had no effect on Rmin in the other soils. A salt threshold of 50–60%Es was found for NaCl and Na2SO4 impacting on N mineralization of Pa-marsh soil. Salt type, salinity level, wetland type and soil layer were the main factors impacting the N mineralization. The results suggest that the effect of salt on N mineralization could vary with salt type and soil properties. Nitrogen mineralization Salinity NaCl Na Estuarine marsh Liu, Yue verfasserin aut Shen, Zhuang verfasserin aut Yu, Miao verfasserin aut Yu, Yang verfasserin aut Wang, Zhikang verfasserin aut Lv, Zhenbo verfasserin aut Yu, Junbao verfasserin aut Enthalten in Catena New York, NY [u.a.] : Elsevier, 1973 196 Online-Ressource (DE-627)30272432X (DE-600)1492500-X (DE-576)081952821 0008-7769 nnns volume:196 GBV_USEFLAG_U SYSFLAG_U GBV_ELV SSG-OPC-GGO GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_32 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_74 GBV_ILN_90 GBV_ILN_95 GBV_ILN_100 GBV_ILN_105 GBV_ILN_110 GBV_ILN_150 GBV_ILN_151 GBV_ILN_224 GBV_ILN_370 GBV_ILN_602 GBV_ILN_702 GBV_ILN_2003 GBV_ILN_2004 GBV_ILN_2005 GBV_ILN_2011 GBV_ILN_2014 GBV_ILN_2015 GBV_ILN_2020 GBV_ILN_2021 GBV_ILN_2025 GBV_ILN_2027 GBV_ILN_2034 GBV_ILN_2038 GBV_ILN_2044 GBV_ILN_2048 GBV_ILN_2049 GBV_ILN_2050 GBV_ILN_2056 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 GBV_ILN_2111 GBV_ILN_2112 GBV_ILN_2113 GBV_ILN_2118 GBV_ILN_2122 GBV_ILN_2129 GBV_ILN_2143 GBV_ILN_2147 GBV_ILN_2148 GBV_ILN_2152 GBV_ILN_2153 GBV_ILN_2190 GBV_ILN_2336 GBV_ILN_2507 GBV_ILN_2522 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4242 GBV_ILN_4251 GBV_ILN_4305 GBV_ILN_4313 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4326 GBV_ILN_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4338 GBV_ILN_4393 38.60 Bodenkunde: Allgemeines Geowissenschaften 38.45 Geomorphologie AR 196
language	English
source	Enthalten in Catena 196 volume:196
sourceStr	Enthalten in Catena 196 volume:196
format_phy_str_mv	Article
bklname	Bodenkunde: Allgemeines Geomorphologie
institution	findex.gbv.de
topic_facet	Nitrogen mineralization Salinity NaCl Na Estuarine marsh
dewey-raw	910
isfreeaccess_bool	false
container_title	Catena
authorswithroles_txt_mv	Yang, Jisong @@aut@@ Liu, Yue @@aut@@ Shen, Zhuang @@aut@@ Yu, Miao @@aut@@ Yu, Yang @@aut@@ Wang, Zhikang @@aut@@ Lv, Zhenbo @@aut@@ Yu, Junbao @@aut@@
publishDateDaySort_date	2020-01-01T00:00:00Z
hierarchy_top_id	30272432X
dewey-sort	3910
id	ELV004910702
language_de	englisch
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However, it remains unclear how N mineralization responses to NaCl and Na2SO4. In the present study, samples of topsoil (0–10 cm) and subsoil (10–20 cm) were collected in three marshes, including a Phragmites australis marsh (Pa-marsh), a Suaeda salsa marsh (Ss-marsh) and a mudflat marsh (Mu-marsh), in the Liaohe River estuary. The soil samples were treated by NaCl and Na2SO4, with a set of salinity levels of 0 %Es, 2 %Es, 5 %Es, 10 %Es, 20 %Es and 100 %Es (%Es, percent of equivalent seawater), respectively. After incubating the soil samples for 2 weeks, the contents of NH4 + N and NO3 − N were measured and the net N mineralization rates (Rmin) were calculated. We found that NH4 + N and NO3 − N accumulations in the soil samples of the three marshes in the NaCl and Na2SO4 treatments. Both NaCl and Na2SO4 significantly affected Rmin for the top soil for Pa-marsh in all salinity treatments, whereas salt-effects for Ss- and Mu-marsh soils were only found at 10 %Es and/or 20 %Es levels in the NaCl treatments. There was an ion-specific effect of NaCl and Na2SO4 on N mineralization. NaCl increased Rmin by 114–164% and 86–139% in the topsoil and subsoil of the three marshes, respectively; Na2SO4 increased Rmin by 234% in the topsoil of Pa-marsh and had no effect on Rmin in the other soils. A salt threshold of 50–60%Es was found for NaCl and Na2SO4 impacting on N mineralization of Pa-marsh soil. Salt type, salinity level, wetland type and soil layer were the main factors impacting the N mineralization. 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author	Yang, Jisong
spellingShingle	Yang, Jisong ddc 910 bkl 38.60 bkl 38.45 misc Nitrogen mineralization misc Salinity misc NaCl misc Na misc Estuarine marsh Short-term effects of NaCl and Na
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topic_title	910 550 DE-600 38.60 bkl 38.45 bkl Short-term effects of NaCl and Na Nitrogen mineralization Salinity NaCl Na Estuarine marsh
topic	ddc 910 bkl 38.60 bkl 38.45 misc Nitrogen mineralization misc Salinity misc NaCl misc Na misc Estuarine marsh
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title	Short-term effects of NaCl and Na
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title_full	Short-term effects of NaCl and Na
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author_browse	Yang, Jisong Liu, Yue Shen, Zhuang Yu, Miao Yu, Yang Wang, Zhikang Lv, Zhenbo Yu, Junbao
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title_sort	short-term effects of nacl and na
title_auth	Short-term effects of NaCl and Na
abstract	NaCl and Na2SO4 are the key factors affecting nitrogen (N) mineralization in the soil of estuarine wetlands. However, it remains unclear how N mineralization responses to NaCl and Na2SO4. In the present study, samples of topsoil (0–10 cm) and subsoil (10–20 cm) were collected in three marshes, including a Phragmites australis marsh (Pa-marsh), a Suaeda salsa marsh (Ss-marsh) and a mudflat marsh (Mu-marsh), in the Liaohe River estuary. The soil samples were treated by NaCl and Na2SO4, with a set of salinity levels of 0 %Es, 2 %Es, 5 %Es, 10 %Es, 20 %Es and 100 %Es (%Es, percent of equivalent seawater), respectively. After incubating the soil samples for 2 weeks, the contents of NH4 + N and NO3 − N were measured and the net N mineralization rates (Rmin) were calculated. We found that NH4 + N and NO3 − N accumulations in the soil samples of the three marshes in the NaCl and Na2SO4 treatments. Both NaCl and Na2SO4 significantly affected Rmin for the top soil for Pa-marsh in all salinity treatments, whereas salt-effects for Ss- and Mu-marsh soils were only found at 10 %Es and/or 20 %Es levels in the NaCl treatments. There was an ion-specific effect of NaCl and Na2SO4 on N mineralization. NaCl increased Rmin by 114–164% and 86–139% in the topsoil and subsoil of the three marshes, respectively; Na2SO4 increased Rmin by 234% in the topsoil of Pa-marsh and had no effect on Rmin in the other soils. A salt threshold of 50–60%Es was found for NaCl and Na2SO4 impacting on N mineralization of Pa-marsh soil. Salt type, salinity level, wetland type and soil layer were the main factors impacting the N mineralization. The results suggest that the effect of salt on N mineralization could vary with salt type and soil properties.
abstractGer	NaCl and Na2SO4 are the key factors affecting nitrogen (N) mineralization in the soil of estuarine wetlands. However, it remains unclear how N mineralization responses to NaCl and Na2SO4. In the present study, samples of topsoil (0–10 cm) and subsoil (10–20 cm) were collected in three marshes, including a Phragmites australis marsh (Pa-marsh), a Suaeda salsa marsh (Ss-marsh) and a mudflat marsh (Mu-marsh), in the Liaohe River estuary. The soil samples were treated by NaCl and Na2SO4, with a set of salinity levels of 0 %Es, 2 %Es, 5 %Es, 10 %Es, 20 %Es and 100 %Es (%Es, percent of equivalent seawater), respectively. After incubating the soil samples for 2 weeks, the contents of NH4 + N and NO3 − N were measured and the net N mineralization rates (Rmin) were calculated. We found that NH4 + N and NO3 − N accumulations in the soil samples of the three marshes in the NaCl and Na2SO4 treatments. Both NaCl and Na2SO4 significantly affected Rmin for the top soil for Pa-marsh in all salinity treatments, whereas salt-effects for Ss- and Mu-marsh soils were only found at 10 %Es and/or 20 %Es levels in the NaCl treatments. There was an ion-specific effect of NaCl and Na2SO4 on N mineralization. NaCl increased Rmin by 114–164% and 86–139% in the topsoil and subsoil of the three marshes, respectively; Na2SO4 increased Rmin by 234% in the topsoil of Pa-marsh and had no effect on Rmin in the other soils. A salt threshold of 50–60%Es was found for NaCl and Na2SO4 impacting on N mineralization of Pa-marsh soil. Salt type, salinity level, wetland type and soil layer were the main factors impacting the N mineralization. The results suggest that the effect of salt on N mineralization could vary with salt type and soil properties.
abstract_unstemmed	NaCl and Na2SO4 are the key factors affecting nitrogen (N) mineralization in the soil of estuarine wetlands. However, it remains unclear how N mineralization responses to NaCl and Na2SO4. In the present study, samples of topsoil (0–10 cm) and subsoil (10–20 cm) were collected in three marshes, including a Phragmites australis marsh (Pa-marsh), a Suaeda salsa marsh (Ss-marsh) and a mudflat marsh (Mu-marsh), in the Liaohe River estuary. The soil samples were treated by NaCl and Na2SO4, with a set of salinity levels of 0 %Es, 2 %Es, 5 %Es, 10 %Es, 20 %Es and 100 %Es (%Es, percent of equivalent seawater), respectively. After incubating the soil samples for 2 weeks, the contents of NH4 + N and NO3 − N were measured and the net N mineralization rates (Rmin) were calculated. We found that NH4 + N and NO3 − N accumulations in the soil samples of the three marshes in the NaCl and Na2SO4 treatments. Both NaCl and Na2SO4 significantly affected Rmin for the top soil for Pa-marsh in all salinity treatments, whereas salt-effects for Ss- and Mu-marsh soils were only found at 10 %Es and/or 20 %Es levels in the NaCl treatments. There was an ion-specific effect of NaCl and Na2SO4 on N mineralization. NaCl increased Rmin by 114–164% and 86–139% in the topsoil and subsoil of the three marshes, respectively; Na2SO4 increased Rmin by 234% in the topsoil of Pa-marsh and had no effect on Rmin in the other soils. A salt threshold of 50–60%Es was found for NaCl and Na2SO4 impacting on N mineralization of Pa-marsh soil. Salt type, salinity level, wetland type and soil layer were the main factors impacting the N mineralization. The results suggest that the effect of salt on N mineralization could vary with salt type and soil properties.
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title_short	Short-term effects of NaCl and Na
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author2	Liu, Yue Shen, Zhuang Yu, Miao Yu, Yang Wang, Zhikang Lv, Zhenbo Yu, Junbao
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doi_str	10.1016/j.catena.2020.104828
up_date	2024-07-07T00:33:08Z
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However, it remains unclear how N mineralization responses to NaCl and Na2SO4. In the present study, samples of topsoil (0–10 cm) and subsoil (10–20 cm) were collected in three marshes, including a Phragmites australis marsh (Pa-marsh), a Suaeda salsa marsh (Ss-marsh) and a mudflat marsh (Mu-marsh), in the Liaohe River estuary. The soil samples were treated by NaCl and Na2SO4, with a set of salinity levels of 0 %Es, 2 %Es, 5 %Es, 10 %Es, 20 %Es and 100 %Es (%Es, percent of equivalent seawater), respectively. After incubating the soil samples for 2 weeks, the contents of NH4 + N and NO3 − N were measured and the net N mineralization rates (Rmin) were calculated. We found that NH4 + N and NO3 − N accumulations in the soil samples of the three marshes in the NaCl and Na2SO4 treatments. Both NaCl and Na2SO4 significantly affected Rmin for the top soil for Pa-marsh in all salinity treatments, whereas salt-effects for Ss- and Mu-marsh soils were only found at 10 %Es and/or 20 %Es levels in the NaCl treatments. There was an ion-specific effect of NaCl and Na2SO4 on N mineralization. NaCl increased Rmin by 114–164% and 86–139% in the topsoil and subsoil of the three marshes, respectively; Na2SO4 increased Rmin by 234% in the topsoil of Pa-marsh and had no effect on Rmin in the other soils. A salt threshold of 50–60%Es was found for NaCl and Na2SO4 impacting on N mineralization of Pa-marsh soil. Salt type, salinity level, wetland type and soil layer were the main factors impacting the N mineralization. The results suggest that the effect of salt on N mineralization could vary with salt type and soil properties.</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Nitrogen mineralization</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Salinity</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">NaCl</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Na</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Estuarine marsh</subfield></datafield><datafield tag="700" ind1="1" ind2=" "><subfield code="a">Liu, Yue</subfield><subfield code="e">verfasserin</subfield><subfield code="4">aut</subfield></datafield><datafield tag="700" ind1="1" ind2=" "><subfield code="a">Shen, Zhuang</subfield><subfield code="e">verfasserin</subfield><subfield code="4">aut</subfield></datafield><datafield tag="700" ind1="1" ind2=" "><subfield code="a">Yu, 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Short-term effects of NaCl and Na

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